Date 0-7639 ERS ITYLIRB lll|llllllllllflllllllfl9llllll will L This is to certify that the thesis entitled Earth Ordovician Sedimentation in Eastern North America: Evidence from the Shakopee Dolomite, Michigan Basin presented by Erin Ann Lynch has been accepted towards fulfillment of the requirements for Masters degree in Geological Sciences Major professor ////9/72 MS U is an Affirmative Action/Equal Opportunity Institution LIBRARY Michlgan State University PLACE iN RETURN BOX to remove this checkout from your record. TO AVOID FINES return on or before date due. f——————_—_———_—_=———__—_—-—_ DATE DUE DATE DUE DATE DUE ___JL________,. l-F MSU Is An Afflrmetive Action/Equal Opportunity Institution ‘ ammonia-o.- EARLY 0RDOVICIAN SEDIMENTATION IN NORTH AMERICA: EVIDENCE FROM THE SHAKOPEE DOLOMITE, MICHIGAN BASIN BY Erin Ann Lynch A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Department of Geological Sciences 1992 ABSTRACT EARLY ORDOVICIAN SEDIMENTATION IN EASTERN NORTH AMERICA: EVIDENCE FROM THE SHAKOPEE DOLOMITE, MICHIGAN BASIN BY Erin Ann Lynch Nine lithofacies representing specific locations within a peritidal environment have been identified in the Shakopee Dolomite (Early Ordovician) of the Michigan basin. These lithofacies and their respective environments of deposition are: quartz arenite, intertidal with an eolian component; laminated anhydrite, restricted shallow subtidal to intertidal; dolomitized mudstone to silty mudstone, semi- restricted to restricted intertidal to shallow subtidal; black-laminated dolomitized mudstone, upper intertidal: fossiliferous, oolitic dolomitized mudstone to wackestone, shallow subtidal to intertidal; intraclastic dolomitized mudstone to wackestone, upper intertidal; nodular anhydrite, restricted peritidal, dominantly upper‘ intertidal to supratidal; intraclastic sandstone, restricted low to high intertidal; and dolomitized boundstone, subtidal to' intertidal. CEl“. Ame anh per thou beer ero and Micr thic Onec This Shai ean Der thic litr An abundance of anhydrite in the Shakopee Dolomite in the central portion of the Michigan Basin is unique to North American basins during the Early Ordovician. The presence of anhydrite in the central Michigan Basin is indicative of periods of restriction. Other North American basins are thought to have been less restricted or anhydrite may have been dissolved or replaced during periods of hiatus and erosion. Correlations based on gamma-ray logs of both the Shakopee and Oneota dolomites were made within the lower peninsula of Michigan. The Shakopee Dolomite shows a dramatic increase in thickness from basin.edge to basin.center'while the underlying Oneota Dolomite maintains a relatively constant thickness. This implies that the Michigan Basin began forming during Shakopee time. Slight periodicity of lithofacies and depositional environment were identified by autocorrelation. .However, this periodicity' is attributed. to ‘the g§0= 0:385 W M. .E hSSh “- m; .A :2: . ocean—8m 3oz 0 :05 302 % 386:0:— Boz m m m... u m a. O a O u d u u 8 m. o o o o w m. w. hon—Bo: m m m a u £338 a 3:: ..... a £528 a 083.35 . so: m 088.2% 33m Boa? O 333.com enouuvsaw osoaoocam 333.com w. W .5."— Eouusum .M m .8... 4m .3... am 5».— .5 ~38.— ..w m Jzncmoom 523qu 5389.3 imam 53232 35:00 1.8— .:oopso-sm 38:... 3.5. ou< $3 .coxE $9 .825 39 .83an use 3.3.... Em '1 > J -‘F’ d 14 1 l L l L 1 l 1 l 1 L4 1 41‘ I Ll 0 an no no on I“ .u . Figure 19A.--Autocorrelogram of first half of sequence of lithofacies grouped according to table 4; 8.--Autocorrelogram of second half of sequence of lithofacies grouped according to table 4 74 M w ”nld 4.. Y‘YI'YIIIWY'YIY'YY‘IYYY'TYYT‘I 0.. "’ ”to“ o I cum-:- ML‘t-u + 1 .1 qr- llellllelILLlJlLllljlllllui rVTrYTYYTYijYYI'TYTIYUTV‘Yifijj IQ 0‘.— JHLLJIAUI11L1111L1111411111Lj11 A. Figure 20A.--Autocorrel_ogram of first half of sequence of lithofacies 3 and all other lithofacies grouped into one: 8.-- Autocorrelogram of second half of sequence of lithofacies 3 and all other lithofacies grouped into one STRATIGRAPHIC CORRELATIONS t t Fost W 3 am a The gamma-ray log measures the natural radiation of a formation. The radioactive materials measured are: potassium, thorium, and uranium. Typically, sands, carbonates, and anhydrites have low radioactivity and thus a low gamma-ray response while a high gamma-ray response, high radioactivity, is often attributed to shales. High gamma-ray response in a sandstone may be due to a high feldspar content (Rider, 1986). In the State Foster well log the gamma-ray response fluctuates. dramatically' (fig. 21). This fluctuation. is characteristic of the Prairie du Chien group in the Michigan basin and is attributed to thinly interbedded Iithologies by Fisher and Barratt (1985). A spectral log is not available for the State Foster well however, one is available for the JEM Doornbos well, which is also from the central basin. The spectral log shows potassium to be the dominant component of the gamma-ray response (fig. 22). Potassium is mainly present _in the Shakopee dolomite as silt-sized potassium feldspars, and illite. Thorium also makes a minor contribution to the gamma-ray response. Thorium could be present in the rocks as 75 76 ICU. M3 SLN/BRAZOS ST FOSTER DEP TH FEET Figure 21.--State Foster gamma-ray and lithodensity logs 77 Thorium Ur "'1‘“ Potassium ) 11700 — 11750 ”—— 118 00 H- _— 11850 Figure 22.--JEM Doornbos spectral gamma-ray log 78 heavy minerals. Although we have no specific data on heavy minerals in the Prairie du Chien group in the Michigan basin, Pride (1966) conducted a study in Wisconsin of heavy minerals in the New Richmond sandstone. He identified garnet, tourmaline, and zircon in the New Richmond sandstone. Of these minerals zircon is thorium bearing. Although the New Richmond sandstone is not present in the lower peninsula of Michigan, there is a possibility that some of these heavy minerals may exist in the dolomites of the Prairie du Chien group and that zircon may make a minor contribution to the gamma-ray response of the State Foster well log. The final contributor to the gamma-ray log is uranium. Organic material attributed mainly to algal mats, is most likely contributing uranium to the gamma-ray log, based on our examination of the core. Uranium can be fixed and passed into sediments through adsorption by organic matter in certain environments. Because uranium continues to be soluble even in the subsurface, its distribution is generally irregular. Therefore, typically on gamma-ray logs, uranium is shown by irregular, high peaks (Rider, 1986). A correlation is not apparent between individual lithofacies and the gamma-ray log of the State Foster core. This may be due in part to the resolution of the log. Units of lithofacies commonly have thicknesses on the order of less than six inches. The gamma-ray log responds to natural radiation from several feet, vertically, of rock. Therefore, the gamma-ray log is recording an averaging of these thin 79 lithofacies units. In determining if a correlation exists between the gamma-ray log and lithofacies units, emphasis was placed on thicker units. It was expected that thicker units of the quartz arenite, black-laminated mudstone, intraclastic quartz sandstone, and boundstone, lithofacies 1, 4, 8, and 9 respectively, would be apparent on the gamma-ray log. Due to the generally clean nature of the quartz sandstones, which contained minor amounts of potassium feldspars, they were expected to have a low gamma-ray response. Thicker units of the black-laminated mudstone and the boundstone lithofacies were expected to have a high gamma-ray response. None of these expectations were observed. The gamma-ray log of the State Foster well does appear to be somewhat cyclical (fig. 21). Table 5 lists locations and gamma-ray values of possible cycles in the State Foster well log. The cyclicity is not explained by correlation of cyclicity in the lithofacies. Instead, we propose that this cyclicity is due to eolian processes in ‘which. detrital potassium feldspars and illite were brought into the dominantly carbonate system. Lithodensity. The density of anhydrite is 2.98 gm/cm?. This value is higher than values of density for dolomite, limestone, and quartzose sands: these values are 2.87 gm/cm§, 2.71 gm/cm3, and 2.65 gm/cm3 respectively. The thicker units of the laminated and nodular anhydrite lithofacies, lithofacies 2 and 7, were expected to be apparent on the density log due to the higher density of the anhydrite which Table 5.--Location and values of cycles and thickness in the State Foster gamma-ray log. chatipn (ft,) Gamma-ray xalQ§_1A211 IniQEfl§§§_lfi£il 11913 - 11943 85 ' 10 30 12007 - 12043 80 - 14 36 12220 - 12268 115 - 25 48 12275 - 12331 120 - 25 56 12425 - 12465 >150 - 30 40 12472 - 12512 140 ‘ 25 40 12515 - 12575 140 - 35 60 12578 - 12638 130 - 35 60 12643 - 12683 >150 ' 20 80 12696 ' 12726 140 - 35 30 12732 ' 12765 140 ' 25 33 80 dominates these lithofacies. Approximately 85% of units of the laminated anhydrite with thicknesses of greater than 2 ft showed an apparent correlation with density peaks ranging from 2.82 to 2.88 gm/cml. Units of the nodular anhydrite with thicknesses over 2.0 ft showed no apparent correlation with the density log. However, other peaks occur between 2.82 and 2.88 gm/cm3 that do not correlate with either the laminated or nodular anhydrite. The laminated anhydrite can only account for 40% of density peaks between 2.82 and 2.9 gm/cml. The nodular anhydrite accounts for 4% of these peaks. Therefore, the correlation between the laminated and nodular anhydrites and the lithodensity log is not straightforward. Again, 81 resolution may play a part in our inability to correlate specific lithofacies units with the density log. Another possibility is that other fine-grained lithofacies contain more anhydrite than identified in thin section.and these other lithofacies are accounting for the other 46% of peaks between 2.82 and 2.9 gm/cm’. Eormation figungazies The contact between the St. Peter sandstone and the Shakopee dolomite in the central Michigan basin is described as slightly gradational by Fisher and Barratt (1985) but can be restricted within 10 or 20 ft. The gamma-ray response to the St. Peter sandstone is relatively low, this is shown in the gamma-ray log of the Martin 1-15 well (fig. 23). The Martin 1-15 well was chosen to demonstrate formation boundaries critical to this study because it is one of the few wells that penetrates the entire Prairie du Chien section in the Michigan basin. The low gamma-ray response of the St. Peter sandstone is followed by a higher, fluctuating gamma-ray response typical of the Shakopee dolomite. The boundary between the Shakopee and Oneota dolomites is represented by a decrease in the gamma-ray response. A similar low gamma-ray package follows the Oneota dolomite. This second low gamma- ray package represents the Cambrian Trempealeau formation. -The thin high gamma-ray response at the base of the Oneota dolomite is described as a shaley zone by Fisher and Barratt (1985). 82 Martin 1-15 Fee 802 “PHI H—l—ll._¢ MPH! 02000 5000 12500 Shakopee ’ Dolomite 7 13000 'T 6000 ‘5 03500 , Trempealeau two Formation 14000 uwwu M um Figure 23.--Martin l-lS (central basin) and Fee 802 (southern basin) gamma-ray logs 83 W Distinguishing the Oneota dolomite and the Trempealeau Formation becomes increasingly difficult in wells located more centrally in the basin. Figure 24 shows the locations of the cross-sections referred to in figures 25 through 28. Where the Oneota dolomite can be distinguished, it's thickness remains relatively constant from the basin edge to the center of the basin. The Shakopee dolomite, in contrast, shows a marked increase in thickness from the basin edge to the basin center. This observation suggests that the central basin began subsiding at a much greater rate during Shakopee time. In some of the wells in the central basin the Oneota dolomite cannot be distinguished on the gamma-ray log. Where the Oneota dolomite is expected the gamma-ray log still shows a relatively high response unlike the characteristic low response in the southern Michigan wells (fig. 28). We suggest that a lithologic transition may occur from the basin edge to the central basin in the Oneota dolomite. This lithologic transition may be an increase in the amount of siliciclastics or organic material. The Cambrian Trempealeau Formation also becomes increasingly difficult to distinguish toward the basin center (fig. 28). This is due, in part, to the difficulty in distinguishing the Oneota dolomite on well logs from the central basin. _One of the characteristics of the gamma-ray log used in distinguishing the Trempealeau Formation is the 84 #! p. I»- Figure 24.--Map showing locations of cross-sections 85 LinSK lulu‘ 8n...- .< ou d Eouu won haulafiaoo no soauaaouuooln.m~ ouanuh 8: 88¢ p I53: um; :13...- l- u 213:».- — 1.35 v .333! .tioJ 2.. 5...! n; it} 86 33o}..— Dug .m 0» m Eouu mooH hmulmaemm MMMMW ' 3.3... w; W O.— 3...? can. L “T— £3508 one: .88. 8:. 838 gr 8s: 3; t3... 8:. m, u to :- .16.: NH.w 09' 8‘ .C...’ 82: m 88. 0% 33...:- MO coflumHmuuooln.o~ Guzman 0.5 '1 ‘.p 3’ 8 87 .0 0» U Eouu mood asunoaaco mo codumHouuouan. a... 5“ 8N: It: \‘ \ j... gr E; coco-l...» 3; ._o u. 30).: . a \ 3.: g: n9; 63.... M M ‘88: en; unto... hm muzofih 2 98 33:35: 071. CE 88 .Q on a scan mood aouumaamm no cowuaamuuooln.m~ gunman { * I l . s/r/ \ 88.1.: [1:1 8: g 0...... 0M 80: g: .3. o: . 83 cm; was... 3 to 33:35: _ _ .I. ,, 8 ~ .. _ . 8.2.88 . 3...:- . .3. 88» ~ _ 8 n k n o 3.. 32.3.. 3.. :8»! 8.3 a; 3...!- z; .83 6.3.... 8: 89 "shaley zone" at the base of the Oneota dolomite described above. The low gamma-ray response of the Trempealeau Formation is then followed by an increased gamma-ray response due to the Cambrian Franconia Sandstone. If the amount of siliciclastics increase in the central portion of the basin and in turn the‘gamma-ray response increases, we may no longer be able to distinguish the "shaley zone". DISCUSSION Depositional Environment Based on the lithofacies identified in the State Foster core and in other well cores, described in this study, the Shakopee dolomite was formed in a peritidal environment. This environment experienced varying levels of restriction and hypersalinity, based on the distribution of anhydrite. Peritidal environments were common in North American basins during Early Ordovician time. The preservation of anhydrite in the Michigan basin however, is somewhat unique. There are three possible explanations for this phenomenon. The first is that anhydrite was present in the other basins but was later dissolved or replaced. Early Ordovician rocks make up the youngest portion of the Sauk Sequence (Sloss et al., 1949; Sloss, 1963). The formation of the Sauk.Sequence was followed by the emergence of the entire craton. An erosional surface formed over much of the craton during this time. However, in many North American basins upper Sauk strata are preserved (Sloss, 1963). Based on examination of well cores from the central portion of the Michigan basin, upper Sauk strata, or the Shakopee Dolomite, are preserved. Therefore, anhydrite is preserved. The widespread unconformity may have reached other 90 91 North American basins. This exposure would result in the removal of a portion of Early Ordovician rocks and it may have allowed for dissolution or replacement of anhydrite. The second possible explanation for the absence of anhydrite is that it was dissolved during cyclical periods of exposure which also formed the cycle caps described by various authors (Koerschner and Read, 1989). The Shakopee dolomite in the Michigan basin is much thinner at the edges than in the central portion of the basin. As discussed below, subsidence is interpreted for the central portion of the basin while exposure and erosion are interpreted at the basin edges. During these periods of exposure, anhydrite was dissolved and other materials were removed. The third possible explanation is that anhydrite was never precipitated in those basins. This again puts the Michigan basin in a unique situation. The absence of anhydrite in other basins of North America with this logic indicates that these basins were less restricted than the Michigan Basin. However, there is no evidence of reefs or structural features which may have caused unusual restriction in the Michigan basin. Regional Stratigraphy The distinction between formation boundaries becomes more difficult in the central portion of the Michigan basin compared with the edges. The St. Peter Sandstone-Shakopee Dolomite boundary is distinct in southern Michigan but becomes slightly gradational in the central basin. The Oneota 92 Dolomite-Trempealeau Dolomite boundary, in southern Michigan, is represented on the gamma-ray log by two low gamma-ray response packages separated by a thin high response package. The deeper low response gamma-ray package represents the Trempealeau Formation while the shallower low response gamma- ray package represents the Oneota dolomite. In the central portion of the basin, the gamma-ray response of the Oneota dolomite becomes higher. The increase in the gamma-ray response is attributed to an increase in the amount of siliciclastics. This increase in the gamma-ray response makes the distincition of formation boundaries more difficult. The Shakopee dolomite is characterized on the gamma-ray log by a high fluctuating response. The increase in the gamma-ray response is attributed to an increase in potassium feldspar. The fluctuation is attributed to the thinnly interbedded nature of the lithofacies. However, a correlation between lithofacies and the gamma-ray or lithodensity logs was not apparent. This can again be attributed to the thinly interbedded nature of the lithofacies. Apparent cyclicity in the gamma-ray log is attributed to eolian processes. Basin Subsidence Basin centered subsidence began during Shakopee time in the Michigan basin. This is evidenced by the marked increase in thickness of the Shakopee Dolomite moving from the basin edge to the central basin (fig. 25). The Oneota Dolomite in contrast maintains a relatively uniform thickness from basin 93 edge to basin centeru The erosional event at the end of Early Ordovician, or Sauk, deposition also plays some role in this variation in thickness of the Shakopee Dolomite. Although there is no‘evidence for an unconformity in the central basin, the southern Michigan wells may show some evidence of erosion. Anhydrite is absent and chert is more abundant in southern Michigan wells. The absence of anhydrite may indicate a more open environment of deposition or dissolution and replacement due to exposure. Basin centered subsidence has been suggested to begin in the Middle Ordovician (Howell and van der Pluijm, 1990). This interpretation is based on upper Prairie du Chien group carbonates, "middle Ordovician", facies tracts that encircle the basin and a thick basin-centered anhydrite facies. We agree with this interpretation however, we suggest that these upper Prairie du Chien group carbonates, Shakopee dolomite, are Early Ordovician in age as discussed in the Previous Work portion of this thesis. HDwell and van der Pluijm (1990) further suggest. Michigan 'basin subsidence is related. to orogenic events in the Appalachians. They cite temporal correlations between major orogenic events in the Appalachians and basin centered-subsidence in Michigan. They describe an early subsidence history for the Michigan basin that consists of cessations and reactivations complicated by episodes of regional tilting. 94 Cyclicity Cyclicity is generated by autocyclic or allocyclic mechanisms or a combination of both. Autocyclic mechanisms originate within the sedimentary system (Selley, 1988). In a tidal setting, examples of these types of mechanisms are migration of a tidal channel or shallowing by carbonate build- up. 'The latter case is more likely for the Shakopee dolomite, in the area of the State Foster core based on the absence of high angle cross-sets and the presence of anhydrite. Specifically, as shallowing occurs by carbonate build-up a more restricted environment results. Restriction may become extreme to the point that algal growth and carbonate deposition ceases. Assuming that subsidence occurs continually water depths then increase since carbonate precipitation no longer keeps up with subsidence rates. Eventually, the increase in water depth decreases restriction to a point that algal growth can again occur and carbonate deposition rates increase. The process then repeats. If this were the case in the State Foster core, cyclicity would be partially defined by lithofacies 4, the black-laminated mudstone. This is not observed. Allocyclic mechanisms originate outside of the sedimentary system. These types of cycles may be the result of climatic, eustatic, and tectonic changes (Selley, 1988). These types of mechanisms include eustatic sea level changes as a result of Milankovitch cycles. The basis for identifying these changes is the rock type or lithofacies present. The 95 lithofacies indicates a depositional environment. Therefore, if a lithofacies is identified that may possibly be broken into more than one lithofacies or if more than one lithofacies exist that could be grouped together, cyclicity may not be recognized. In Lower Paleozoic rocks, before the development of extensive infaunas or browsing organisms, sedimentary laminations may have been preserved in all tidal environments (Shinn, 1983). In this instance, the lithofacies 3, laminated mudstone lithofacies, may represent more than one environment but there may be no basis for breaking it down further. Allocyclicity may not be apparent in this situation. In the State Foster core, cycles are poorly defined. Part of this may be due to the lack of exposure. This is supported by the abundance of evaporites and the lack of exposure features such as mudcracks and teepee structures. Burrowing is also relatively rare which correlates with the abundance of anhydrite indicating restriction. Peritidal cycles have been recognized by exposure features in lithofacies capping 'tidal packages (Koerschner' and. Read, 1989). Subtidal cycles have been recognized by a gradual increase in the abundance of storm beds as shallowing occurs due to carbonate build-up (Osleger and Read, 1991). There is a lack of distinct subtidal sedimentation including.storm beds in the Shakopee dolomite of the central Michigan basin. CONCLUSIONS The State Foster core represents a peritidal environment of deposition. Nine lithofacies, corresponding to specific areas of a peritidal environment, have been identified in the core. 'These lithofacies are: quartz arenite; laminated anhydrite; dolomitized mudstone to silty mudstone; black- laminated dolomitized mudstone; fossiliferous, oolitic dolomitized mudstone to wackestone; intraclastic dolomitized mudstone to wackestone; nodular anhydrite; intraclastic sandstone; and dolomitized boundstone. Their corresponding environments are: intertidal with an eolian component, restricted shallow subtidal to intertidal, semi-restricted to restricted intertidal to shallow subtidal, upper intertidal, shallow subtidal to intertidal, upper intertidal, restricted peritidal dominantly upper intertidal to supratidal, shallow subtidal to intertidal, restricted.low'to high intertidal, and subtidal to intertidal respectively. The abundance of anhydrite in different lithofacies of the Shakopee dolomite of the central Michigan basin indicates a restricted environment of deposition. The absence of anhydrite in the Shakopee dolomite at the Michigan basin edges and in equivalent units in other North American basins, may'be 96 97 due to a less-restricted environment. An elongate basin from the Black Warrior to the Michigan basin may have existed. The Michigan basin frequently became semi-restricted to restricted, due to the size of the tidal shelf, while the Black Warrior and Illinois basins remained more open. Another explanation for the absence of anhydrite is dissolution or replacement during periods of hiatus and erosion some of which may be associated with the craton-wide erosional event at the end of Early Ordovician time. Lithofacies identified in the State Foster core show no straightforward correlation with gamma-ray or density logs. Cyclicity in the gamma-ray log is thought to be associated with eolian processes. Correlations made within the lower peninsula of Michigan using gamma-ray logs showed a dramatic increase in thickness of the Shakopee Dolomite from the basin edge to the central basin and the relatively uniform thickness of the underlying Oneota Dolomite. These correlations indicate the Michigan Basin began forming during Shakopee time. Cyclicity within the State Foster core was identified by autocorrelation. However, cyclicity is due to the dominant frequency and thickness of lithofacies 3, dolomitized mudstone to silty mudstone. APPENDICES 98 List of Abbreviations--Appendix A @ abnt abv aft Alg alt alt'g amt ang anhed anhy app aprox bcm bd bdg bf bioturb bl blk blky Brac brec bri brit brn bur c calc cgl chlor cht chty cl cln clr cmt cncn col com conch ctc -decr defm. dess dk dns dol At Abundant Above After Algal Altered(ing) Alternating Amount Angular Anhedral Anhydrite Appear Approximate Become(ing) Bed Bedding Buff Bioturbated Blue(ish) Black Blocky Brachiopod Breccia(ted) Bright Brittle Brown Burrowed Coarse(ly) Calcite(areous) Conglomerate Chlorite Chert Cherty Clastic Clean Clear Cement(ed) Concentric Color(ed) Common Conchoidal Contact Decrease(ing) Deformed Dessication Dark(er) Dense(er) Dolomite(ic) dtrl elg euhed f fib fis fl flt fltg fnt fos frac freq fri 9 Cast gn gr grd gy horiz homo hvy incl incr infreq intbd intcl intlam ireg lam len lrg ls lt lwr mas mat mot mtx nod nr Detrital Elongate Euhedral Fine(ly) Fibrous Fissile Fill(ed) Fault(ed) Floating Faint(ly) Fossiliferous Fracture(ed) Frequent Friable Good Gastropod Green Grain(ed) Grade(ed) Gray Horizontal Homogeneous Heavy Included(sion) Increase(ing) Infrequent Interbedded Intraclastic Interlaminated Irregular Laminated Lenticular Large(er) Limestone Light(er) Lower Medium Massive Material Mottled Matrix Nodule(lar) Near occ Onc ool org ox P pbl pel phos plan pos pred prim prob pt PYr rad rd repl resd rr s scat sd sdy sed shy silicl sl slt sltst slty soln srt ss stromlt strc styl subhoriz surf sz tab tex thk thn thru tr 99 Occasional uni Oncolite up Oolite Organic v Oxidized var vert Poor(ly) Pebble w/ Pellet w Phosphate wh Pink Planar xl Possible(ly) xlam Predominant(ly) Primarily y Probably Part(ly) zn Pyrite Radiate(ing) Round(ed) Replac(ing)(ment) Residue(a1) Rare Small Scattered Sand Sandy Sediment(ary) Shaly Siliciclastic Slight(ly) Silt Siltstone Silty Solution Sort(ed) Sandstone Stromatolite Structure Stylolite(ic) Subhorizontal Surface Size Tabular Texture Thick Thin Throughout Trace Unidirectional Upper Very Variable Vertical With Well White Crystal(line) Cross-laminated Yellow Zone o.¢vwdd 101 camp won am can .oaon. 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Ascovs.mooss o ansx .Aucecusn .somuucscooc can ~.mowss. sass ado .anH an u > \3 so DH no u oso: oHao .so eIua I. nan use .Ema xsa Asm~.c as .so: sacs omuomoeoo xnu so 2 ans osmo nun .so a moossI o.nooaa and an» > usm vHoo I ~.novHH Anne >vusn .ABMH nossIsncm .so uHVEmH ono so ya .sua I 107 nosaa w Acmm.uvavx an .EvH noun uuo> .svx Hov u sun .No xv nooHHI m.~oodd uoa xov u nun .so xv I mvoo no so xxn meow can o.xosxs vcv aux xxn xgm~.c.xn.xosxx v mcvcmsvmm :xom "no u .so xv .so I n.uosnx pan xov sIv so as I .I v.oosxx mavom :Hom .moaxooam an nuo EIu so xv .s: I v.oosua avx nus v > xov u so xv I n.oosHH mavmm cHom .mmaxooum xan Nuo EIu so xv .:3 I can Eva an 020m \3 Eva u > gov EIu .so uHIB oosaHI o.oooHH xcvxmveva sacs u so OHIB I .m.oomHH son .va v xov v squn uxIa I oovsx o xso xxvvcvoc sncv n.oovxx .xgmm..n vcv s.oovsx o Agm.xcavx xxn .uvn .uoe xov 8 sun .so a I no swo m.oovxx mfivmm saom uvo EIu xv .sun I H.moona oaoz mam .uao scam .Amannma uvaVHUHCs scam .Hov u so a .I— 108 £3 vandal moon @ Henna .EvH omuw Hov .nuo u .squn I x.nxsxx Aucavauv vow uuou .msmmm :Hom .va omus Hov u so va3 I x3..so v.~usxu_ avx uos uov .uuo aIu Iun uxI: .I_ so.xv . .sm. 0» a: .uuuquuacuoucu .xucvcavxx ouvo .uuo aIu .cua .so «usqu_ ~.xusxu aux xxu gms. .xun u vcv so xsuvavx ouvo u un .so a I u emu uuu uoa ouvo u Nquu a Husqu v.oosuu a su vcv m.oosuu o gm. aux vo: u .xxunc ovum .x.oxsxu o :N .o.oosuu o .ms.x .n.oosxs m.ousxx_ o gm. “gm o» as .axunoo uvuucavu soucu .svu uuu oxvo u so a .cun I” u.oosuu_ 0E0: Davu .Nuo EIu can .s: I xcvuoc2vu ouvo u swla .cun oosqu ‘ sncv x.sosux v0: scam u uxo .mevom :Hom .oamu u so E .sun I o.vcsux mEvom :Hom Damn u so E .sun I. and omun uum> .xcvxnvfivx Davo u so a .sun oosaHI. ~.evsxsb ouu usx o soucu .xucuesvx oxvo u sun .so xv I“ nun «.sosxu qu an Ho .mevmm :Hom Oxvo .Nuo EIu .so HAInz . I 109 m.VNhHH xoou xnucavx uov u so a .cun ox am anonn sun ~.v~sua .xan as» van so a xsu o.uan soous unz3oaomvanx Oxno .Hov u .so vaI I m.nNsHH, omnn w wuso x0 \3 050: Hov u xun I n.-sad w Hmum .Euv vow umoo Hov u Nqun vaE nusunl~ so n.-suu. Aucavuon .EnH squn B owusu0«e \3 o.an .EnH Nuo EIu Inn a .s: I nun vows: 2 ans xua .zm.ce .soo Houcu u .xunvavux ou ose: uuo aIu .so xv .:3 I I m.o~sux mason axon .avx xxu xgm.c¢ .xcvuocsvx xov u nun .so xv . I ans xuu Asm~.c~ .uvn .avu uov u sun .so xv ousqu owns 9 doves u no mxsdsud .amn v05 unzsoeoo .vo: szcn oouMCM .menom cHom uuo u E .sun .23 I uoxxo co «.vxsuu ans u ovuu .suucs uoe .xov .Nuo u sonv .so I uoxxu co n.vxsuu M ens u > .uov u squn vaa I HOHr—U :0 N oGHFHH _ ans u ovuu .xoucs uos .xov .uuo u Iso xv .so and oouw coqunvo use .Enx oous Hov u mo 6 vHsHHI H.¢Hoaa ens xxu u use .snx uuo u no I 110 onhddl oona w aOsuIsaan voa .an uau. maan .Hov u mqua xv oona w voa van manom muonsad axon .xaov xounanvanx xxa .Auaavusa .EnH anxm Hov u so a .aua I and ausquaan u > oaom \3 oaoa Hou maan .aov u mqun an onsHHI “ ~.~nsax I m.~nsaa soup aoo n.mnsau and xxa .xuaavuan .oouvunou muovvooua uuo> .Enx Hov u «a .so xv I _. H.nnsdnm voa saan soIHa ox oaom .Enx oous saan .Hov BIu uaIso vaa II ans xun \3 ans ausuInuo uuo a nun .az. onsqu ans uos meow . o.o~sux. .aoo ans aoHquuo .v.o~saa w Asavsnxx .anx anxa Hov u auaIso xv I. no ousm 3. v.o~sda Ivao aux: ma uo u van ans aosuInuo .an oous nuo EIu .squa ad I m.v~suu. soucu uuo aIu :3 .xxn I_ v.v~bHHm voa \3 manom axom anu u so vaa I xoouuasvmfinom axon saan W xuu .x00 u .xxu gm ans soucu .voc sxcv u uuo .ouno u so qua vusqu o.m~snu_ manoo axon .Enx voa vouonmaoo Aaau van xauvanx Hov u so a .aua I e.m~suu o Ascvcsnxx .svx v.m~sux xun xsmu.cm .cau vcv xxu o.uxv ovuu smucavx uov u so a .cun I. «.mmsxaw manom axon .anx voa vouonaaoo xaau van xauvanx xov u so a .aua I 111 ¢.v¢sHH oaouovoa squa mo mumnao \3 oaoa Nuo EIu qua .a3 H.vvsaH. soucu .uos uuo sIu squn..a3 I, ND . voa Mao aIu Iun a was evoHHI . o.nvoaa_ aux uo a van u o.uxv u xov aIu so xv I s.nosxu, soucu so xv u neon uuo u gun .a: I so 921.3 W vouonaaoo .voa ausuIsaan .uoa saan .Hov u Ian a .m& I evu ago an» uov u cunIso xv nesqu w.~vsHH_ and voa Hov u auaIso xv . I. , v.~vsxum oaoa oHno u auaIso xv I . v.~vsxu _ soucu .cox uov u cunIso xv . 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I Sons:m xaHu usn \3 oaovvoa saan HHsv so uH oH .anH vuo oHno so vaa I can eouu gmm. xouov ouo «.vmsHH oaH3oHHou BnH usm u > \3 090 uoon oouH .osoa Hov xHa I «.vmsHH avH ucu Hov so aIuH I H.vmsHH Emv vow uuom .mEnom aHom .voa Hov so EIuH I , o.nmsHH uvu .=m~.uoomnu o ans o xv .svH ucu Hov so sIuH I saan a: on uHo \3 o.~msHH w ouo oouH .oaoa Hou Hov so vaa nmsHHI Axon xouoavvsoo avH xHu .ooun uuo> on“ v.~msHH van.EnH oouH una3oaom aoau m.HmsHH ou EnH anHQ Hov .so a .aun I 114 o.nbhHH svm .anH anus aau nuo u so xv .an n.ussuu o Honu saan .ussuu on m.ossuu saan «a m.nssHH _ o oouH Boa .saan van Hov aH van mo BnH o.an .Hov .nuo aIu .so UH .a: I . . saan «a .so m.ovsuu xua a: sauoanu as .u on on oIHa van aacuouau .Hov .nuo aIu IxHa a .a: I, on ~.ovsHH _ onoun aoHuIsaan oIHa van anH ua .anH oouH saan .Hov u .so aIuH I, oona vunsou Hov uoaH van oav aH uoaH manom aHom s.ovsHH .voa .voa voaouunHu .vouonmaoo voa aoHuIsaan Hov .saan u so vaa .I H.vvsHH anH anHa Hov u so vaa I n.nnsuu o gs .n.onsuu o =m.u II o.mvsuu manoo aHoo aoHuIsaan vouonnaoo voa .EnH uau Hov u so vaa I I. H.evsHH m.nvsHH w Eon .anH noun uuo> oaom .EnH anHQ Hov u an .so uH I an n.nvaH oona ua voa saan .xHa aoo anH u > Hov u .qua xv I_ an. , uo a unom .Houau .uoa saan .uov aIu .o IHa uH nvsHuI ua n.~vsHH ans squa van on o.uun .anH anuo saan .Hov aIu .oIHa uH I . «.mvsHH” uoa .aoqusaan Hov u so IHa uH I, on .so . ansuIsaan voa uoa Hov .saan u IHa aIuH mvsqu 115 nan saan as on use .umno xua H.~nsuu .onum moan .aoH oHuHuoHa.:m~.H on a: HouaH oHno .so xv .a: I I oHuHuoHaNo xv van vouonmaoo voa so uH o.an anH oouH Hou oHno so vauH. «noHHI m.HnsHHW anH anHQ uau oHno so vaa I” sanH uam nonvoaoa oHno so a HosHHIM m.oosHH EnH aan can > uau oHno so vaa I, ,so _ EnH anHQ aau Hov .saan Iaua vaa onsHHI, o.nssHHW EnH aan aau saan so vaa . I . H.nssHH voa saan .Hov xHa .so a I voa vouonaaoo \3 Anoun mavvmanom aHom saan .Hov xHa .so I nooHHI“ ma o.ossHH anH onus oouH saan .Hov uH .so vH I «.sssxu .m.vssuu o anu uoa .xn.ssssu o =m.~canu soIHa v.sssHH vouonaaoo voa .oIHa uH van «a o.an anH aan saan .Hov a .so aIuH I, xv.mssuu soIHn H.vssHH a anvvoa maan soIHa \3 oaoa .mou w uuam xo saan .Hov a .so aIuH I. m.mssHH auv vow m.mosHH uuom “o.vosHH .m.vssHH manom aHom so noun mav saan .Hov so aIuH I_ van .saan Lv.vssHH uoa oH suaov.omna ua voa ou anH uau .Hov so xv I uoHao oaoo. mom «n.~ohHH 0» oHosHH .n.oosHH 0» m.oosHH «.HosHH aouu sHHnHoomoo usa “aunov \3 uau Eon anHa anH Hov u so aIaH , I a ,I am. 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EnH aoHquuo xHa oHno u so a .xHa I «.vosuu sue svo aaH\3 Hsum xaoHvHouaH oHno EIu so a I =m~.u on o: .3Ha una aouu o.nnsuu o unuas .usum 0: .xanx uau > monsoaoa ouno aIu so vaa ensHHI v.nnsHH_ usum \3 ans can > uau oHno u so vaa I_ 500 Hou Hsum No m.nmsHH . xHa uuo u uo a 2m.H on an HouaH “uHo saan voa oHno SIM vaa .a: I xua oHuHuoHa no .umno xHa n.~osHH ..onum moan .aoH oHuHuoHa :mm.H on a: HouaH oHno u .so xv .a: I_ 117 swanow aHowvanH u so Iaua a van anH voa so aIuH o.an .EnH oouH Hou oHno u squa va3 nosHHI waoHunuaoHuo m.oosHH un> .voaouunHu voa o uH .AanH vuo uau nonvoaoa oHno u squa vaE I o.vosHH_ anH uo un> .uau oHno u squn vaE .I . v.mosHH_ anH anHa Hov .saan ,u so.vaa I I. . «.vosuuw snoun wavvwanow aHow “anH u > Hov u so 9H .xHa . .I_ :mm. on am.H sous u «.vosHH_ un> .una uo u van HXIouoHa o.an .anH anHa uau Hov In > so EIuH I_ usm .Hov o.nosHH_ EnH anHa .saan u so vaa I H.nooHH oaoa nuo E as I . maIaua ans uo a nuoa .anu u onus Hou uau uov aIu .so a .xHa nosHHI I . uaIaun o.~ooHH one no .auv vow unow .voa Hov aIu .so a .xHa . I, uaIaua v.~osHH aoHuIsaan .wEnow aHow u saan .Hov EIu .so a .an I aoHqusa uaIaua. «.mosHH .wanow aHow aoHquuo xHa \3 .voa .voa vouonaaoo Hov u .so a .an I. ma «.HosHH anHQ u EnH Hov u Iaun .so B . I_ 118 an a «.vonHH Huou saan wnoun so xv \3 nos saan .Hov u IuH .so xv I owna . v.~omHH ua auv vow vuow \3 voa Eva “xau un> .anH oouH Hov u so EIuH I uoua oouu anH an an «.monHH uaOHquuo nun .so a .a: o.an .una .anH oouH > uuo .Hov aIu .so uH,.a3 I m.HooHH aOHquuo .wav .wanow aHow Hov u xHa . I «.HonHH xau un> .uau .anu onus uov u so vaa I so wnoun vouHHnooH aH wanow aHow .AuauvHouaH .voa Hov u xv .so uH HonHHI uaa .aoHquuo wanow m.oooHH aHow xHa “anH voa oaHauou u Hou saua ma xvvvoa oHno u «a xv .xHa I v.oosHH w EnH «.vooHH uoa .gm.ucxau “.m.~ on an. xau un> ans anus uau ouno u xua .so xv I an m.oosHH aoHquuo xHa wanow aHow .voa u 0Hn0 u .so BIaH I n.oosHH H.oosuu o .ms. noun onuu .anu anuo u uau ouno u auaIua a I s.nosHH .m.nosHH .~.nosHu o .=m~.H.n wuwnHo vavou uo a uo u \3 ma van :3 .Hoo \3 EnH HouaH oan “EnH u soIaua xHaIua a van anH voa so aIuH o.an .xau un> EnH oouH > oHno EIu .so aIuH oosHHI 119 QOU o aua oaoa “owna m.oooHH ua wanow aHow aH\3 voa so HHsv u \3 wanow aHow Hov u squa xv . I n.oonHH ans aoquouo xua Hov u xua I so UH .aun «.sooHH anH so van aua o.UHn .anH aan Hov u «a vaa I so uH .aun o.nonHH owna w vaaoa oouH .aua ma xv oaoa Hov u an vaI I o.nooHH anH anHa saan u oIHa xv I auaIua voa so uH Huav uaa .uoa Hov u a .so a nonHHI Amav unuoaoquouo xua auaqu n.5onuu wanow aHow :H Hnwna nun van so o.UHn .EnH anHu Hov u a .so a I ans anuo saan u xHa .so xv sonHHI .uaa. H0 ua voaoUunHu oaow \3 wnoun wav snow an n.vonHH .aHow scm.vaaU van anH osoa ma saw 0U am.HvxaU Hov u .u& .so UH I anH vuo an anHUva . o.mowHH ouoa “wanow aHow swav anvaaU .aoHquuo ouoa Hov u xHa .so UH I n.monHH uo .Uau .anH oouH Hou Hov u so UH I Eon oouu xHa van a: .ua o.UHn anH aoHquuo .wanow aHow .wavoxHa .gm..n «.monuu on s.nonux “v.nonuu o a: .un a «.monHH an anH svw uo a .vuo Una anHUva .anH oouH Hou Hov EIu IUH .so xv I 120 . so . auaU Hoo .onun moan .sm. 0U u > Eouu oaHoanu Iaun vaE s.mHoHH Ho so xv nu a HHav vu .xua aouInuo \3 Houau ouno .nuo u .so uHIaa . I wEnow aHow \3 . vuo usu o HouaH .voa so on Huav nu unom \3 ans so uH «.munuu oaoa so a on xv “oou o ans aoquouo xua .mn. Hov u .so vaa I «mu aoquouo .anHH van m.munuu o uon .aun aunIan m.nHouH an xv van so UH o.UHn .EnH anHa u sHHnuoaoo oHno .Hov u .so.EIUH I v.nHmHH Uau EnH aan oHno .Hov u soIaun E . I wEnow aHow \3 UOE oHnu .Hov u soIaun xv nHmHHI u > voa “Enow aHow n no v.~HmHH. aoHUoow vanoun noun aoHqusm .wEnow aHow \3 UOE saan u soIHn EIUH I. ~.~anufl 0E0: oHno .Hov u soIaun E I , o.HHoHH_ Uau Hou EnH anHQ u > oHno .Hov u soIaun xv I” . . .v.HunHH. oaoa ouno .Hov u squn uH . I noun aUHqusm . «wanna axon aunIxua \3 Houau so nu voa .aou auaIan m.anuu ua uan uaE .aUnov \3 oouH ouOE Eon EnH oou Hou oHno .Hov u .so UH I H.ounuu o anH =m.n aux; unow voa - so as uuvv .ounuu o .u aoquouo xua .v.oonsu o voa so as quv u \3 wannm auow =mn. .auaIua xHaIso a «.vunHu, uo ovnaw as un> xau :ms.n on :u aouu ans vuo vuno .Hov u .aun on xv I. 1.. 2 1 Hoo .aoHuIsnan won .wEnow aHow Uau oHnu EIu so vaI onoHHI . o.o~nHH Hoo .UOE .HanH Unow oHno .nUo E so EIUH I on m.o~oHu aoH an oHo \3 UOE “EnH anHm u > aH oou oHno u .so vaI I . un soc .voa oHnu a\3.u .so vaa ounHHI v.n~nHH EnH anHu saan u soIHn vaE I ‘ an :H Hnwnn aH wEnow aHow oEow “EnH an .so EIUH n.v~oHH van so uH acqunuo a van on u o.uun .anu anHo nuo .Hov aIu .squn xv I anH aosquuo xun van ans xun n.m~nuu squn xv svvouo .som aoquouo xun .anu anus aau Hov u .squn xv . I nnnxu o .m. \3 non aoquouo xxa .anu . squn uoa «nous o .m.u .anH vouonoaoo voa oaom on ouoa .anH «a van .so xv .so a o.an .anH anHo Hov u a .so vaa nunHHI uva sn noun oouu soon u on as n.u~nux oan uuo u an UH van so E 0U UH o.UHn .EnH anHQ .nUo EIu .so EIUH I . an ax xsavom.nunus o an anux .xau un> anu oouu > .uoa nuo aIu .so nu > oHnHuI gmn. on so a .xHa n.nunuu a: voa .m.anHH 0U a: u > voa usunU wEnow aHow oHno u .soIaun xv I EnH aan so UH .an H.vHoHH u aoaU QOU w ans. 0U a: H0 aoH van wEnow aHow oHno u .squn UH I -Iso >an anau uann nooH u H0 .xua aosuInuo \3 Houau ouno .nuo aIu xv .so uH nunqu EnH aoHu v.5noHH Iouo xua cm. .aoH anus an» > .un oaoa .m.~ on Hov u an .un I v.nnnuu voa an H > .Eoo wEnow aHow aoHquuo xv Hov u un .an I_ onuu onum .wvHoaHuo Haou snan m.vnoHH oH «Hoo “nOHuIsnan qunow aHow uxuvvoa «HOUaH Hov EIu so vaE I ans. QOU w XUE uo E \3 EnH HOUaH aau .anu uo a van u o.an oouu .anH anuo aau Hov .nuo aIu so xv .an mnnqu . n.nnnHH. UOE nUo EIu so EIUH I EnH anHa u Hov u ao .so E vanHI on n.nnnuuu auv von noon .xuau nan uoauuwuvoanu oouu aau Hov u .so aIuH I on pH van so uH o.uun .voasunsv uvn nauoanu anHo aau H.nnnuu aoau .nnnuu o aau aoHquuo xua aoau .Hsuw .sxua Hov u unIso UH I. vaaon a: o auov vow uuon .xua n.~nnHH a .uo u H0 .voa un oaoo .anH aau onuu .Houas Hov aIu on pH .an I I . m.HnnHH AwEnow aHow UaHVOan nUo EIu an I_ on n.unnuu auv vow uuow .uoa nuo aIu .so uH .as I n.unnuu, Hoo .voa .UOE oHno u so EIUH I. H00 .vuo usu n sxunuooooo m.onnuu oouu HsUw .QOU ua XUE aoHuInUo E .UOE .HanH oHno .nUo EIu so vaE I, 3 2 1 v.vmnHH a uoan aoHquuo xnU an. oan “anu “XUE u svnavun oan «.vaaon H0 wonHouv HsUw “UEU snan a3 OU uHo .Hoo .st 0U QaVHOUaH oHno DIE so E mmoHHI voa uo UEo a: 0U uHo aoHuIsnan “HOUaH no wuoan oUnunaow OU nan oouu HsUw .wEnow saan v.vmoHH aHow .Hoo .svoUuonnaw Ho wavaanH .xaovaoa .oHno u so.E I n.~moHH Hoo won .EuOUo oH .waoHUnUaoHuo HHn HOIQHu oHno u so E I oaomnHH svoavaoH uo E u Unow swEnow aHow UaHVOan Hov u an I wH II van Hov EnHuanH an Hnwnn .AvoavaoHUoow no QOU o aoH ouoa .uvn uaa > .nmn xau gm. on a: anH ~.omnuu aoquouo an van so xv o.uun .anu anuo aau > ouno .uov u so xv .xHa I an .aun s.ovoHH onnuu o .mn. ans anquouo an \3 oaoa uov u .so xv I un xv .an o.nvnHH EnH anHa Hov u .so xv I ownn ua usn an UH «.mvaH .xcH 0U a: onuu .uo uvHanH .xUE svw aoHuInUo Hov .qu EIu .so UH .a3 I n.nnnHH o gmn. ans aoquouo ,II n.nvnHH xun an» > .anu uo a van u o.uun .anu oous u > uov aIu so xv .an I so EnH uo E aoHuInUo oEow oan “EnH anHQ saan u soIHn vaE vvnHHI uo E Unow \3 u sHEov s.oanH 3oHon “EnH s.ovaH uo E van u o.UHn .EnH oouH Uau “UOE :m.n a: nUo EIm so EIUH . I 124 an xv unn uaE “EnH anHu xaU un> Hov EIu .so vaE ovnHHI ownn n ans. sHHnuooono aoquouo an .u.nnnuu o anH an .n.nvnHH anU stn oan “unn oEow “EnH anHa vuo Uau xaU Hov u .so vaE I. . an o.svnHH usn oEow «won aoHquuo “EnH anHa aaU Hov u .so vaE I. an m . svoHH EnH noHqusa u > «noHquuo “EnH anHa anU > Hov u .so vaE I, . m.mnnuu o an H.nvnsu an wEnow aHow .aoHquuo an “voUonano voa .UOE Hov u .so vaE . I, EnH noHqusn u “voa u «n . on Han :m.~+ «uo E Unow .unn “EnH Uau xaU un> Hov EIu xv .so xv mvoHHI unn “non Eoo EnH noHquuo an .EnH anHa Hov u an xv .an HonHHI n.omnHH_ EnH anHa Uau aaU > Hov u so E Im ownn o gm. ans aoHquuo an V xHu .uvn .anH uo a van saw u o.uun ans anuo u Hov aIu .qun as omnHuI UnE aOHquuO an an n.9mmHH no ovoo \3 uoa .sxua on aoxoun one on u one o Hov aIu .squn on I. xgm.u on on no vouuoooam ~.nmnHH_ xua uo u on .xvoHouas .aosuIsaan .xua oaoa ,Hov .nuo oIa on xv .an I. . use xgm.~v “ voa saan a3 0U uHo oH > oan smmHH @ uo E Unow M Eon “Euv vow Uuow “uooH sHUnoHHw voa “n.0meH . M oouon Hsuo won n.nmnHH .nmnuu .n.mmnuu n.smnHHm o HsUw so oan “voa oaHsoHHou HsUw “Awavvvoa u Hov EIu aunIso xv I“ 125 m.nsnxu o anH uo a neon n.nsnuu «nUaov \3 anHUva ouOE Eon Uau .EnH anHo aaU saan u soIHn xv . I m.~anH. wonuu uHuon “OEon Hov u an . I v.HsoHH. Oan “wEnow aHow Hov u an .so xv I ans xun .uva “ans Hov u an .smrxv HsoHHI s.osmHHq suavvanux Hov u an .so xv I , n.osnuu. 0an qunow aHow Hov u an .so xv Ih an m.osnuu aoH 0U voa “wEnow aHow “EnH Hov u .so vaUH I, n.csoHH onum “HUUaH “amm. voa saan uHo oHno u so EIUH I. N.ObmHH onum .u HUUaH “UOE “Han voa u “aoHuIsnan Hx oHno u so E I EnH H.osoHH anHUva “uan “EnH onuu .onuoama sHUnoHHo .EnH Hov u so vaE I HOUaH “um EnH aoHu un xv H Iouo an anU «nUaov \3 UOE ouOE Eon “voa u Han oHno EIu .so vaE oanHI ua xv n.ovnuu an \3 oouuaH voa saan uHo “u HOUaH oHno EIu .so vaE I un xv ~.ovnHH. Euv vow Uuow .EnH UOE Hov EIM .so vaE I 126 FQQHHI noHuIsnan EnH voa snan u so vaE . s.nonHH anu .voa saan Huvv u .n.nnnuu o gm Houau uov u so vaa I ownn . m.vooHH w susw so “Hoo uxnU am. EnH snan voa HHav u saan u so UH .I, . n.vooHH v.mmnHH a onum .ano «Hoo “HOUaH uosoa Hov E an I. m.nwwHH o .m. aoqusaan oaoa xHa “wnoun o auv von noon on H «unn oEow «uo E van u o.UHn EnH oouH UnasoEow Hov EIu .so EIUH .mnoHHI «.oanHm noHuIsaan «unn «UOE Unn3oEow “EnH oouH Hov u so EIUH I. :mm. uHo voa H.osoHH saan “aoHuIsaan uxEnH an onus EovaanH «UOE Hov u so EIUH I aoquuouuun .anu onus sou nuo aIu squn nu osnuHI. o.sanH noHuIHoHHHo “OUO Hnwnn ua HanH Eon noHuIsaan NUo .saan E an In v.ssnuu on s.msnuu aouu uo a .msnsuxgm.~c .n.msan..Ho n so on oaoa wanow aHow .anH uo . n.sanH u so xv van so an .nuosnu xuuavcsaan voa a anu Hov u so vauH . I_ n.vonHH, uHo voa snan “onum woaa “HanH Hov u so E I wHu “woovo voauaUmn \3 . o.vomHH_ EnH an oEow “unn oEow “aoHquuo EnH an oouH u Hov u so vaE I, w - H.282w aoH am. voa saan uHo “oaoa nan .EnH xnU Uau > Hov EIu so E . I. 127 n.oooHH ans so as uo a vnn ans on uo u .anH Hov aIu so uH .un Hov .saan :3 n.nooHu svn .Houau .soIHa. voa n.noouu .nuo aIu .soIHn .un. I . un auoov \3 ausuIsaan ouoa van xau non .anH saan .Hov .u .so aIuH vooHHI one II on on uo u no voa onus vouonoaou \3 .anH uau .uoa Hov .saan u .so Hnva nvoHnI n.nooHH ans uau .uoa saan u so Hava I saan sn Haou oaoo .uo u oun ans on on .an n.nooHH «ownn a HanH uo u uaE .Euv vow Uuow .EnH oouH nUo E .a3 .so UH I m.~ooHHx=m~.o .o.oonHH.=m.. aon .ooonxsvv .~.oonuux:m.nv .n.nonuux=m.~. anH voa .n.sonux o Hoou saan Ha \3 nos .~.son~H o uvn aoHHnao > uaa .n.sonHH .m.vonHH so o.~ooHH a ounUnou vonunaaaov “Euv vow Uuow «EnH oouH Hov u .«n EIUH I n.monHH u anH aoquouo an .n.monnuxgm~.v EnH aoHuIsnan uo E Oan an “v.vowHH ouaUnou voouosov .n.nonuuxcm~.. .n.nonxux=m~.o anH saan :3 on uHo “nooHH noov anH ausquao onuu sxun Hov a\3.u squn UH nonHuI ans aoquouo uov u an nonHHI ownn w Euv vow Uuow “m.~onHH o .H anH uHo .uuo oouuau voa saan “gmm. o.~onuu wonuu EnH oaHvsHoaH Auo E oaHnonoumanv HanH Hov u so E I . m.oonHH o =m.u . nu. unuas .aoo Hou ans aoquouo xua .so». use n.HonHu voa saan oouuaH “usn “Eoo Euv vow Uuow “EnH voa Hov u so E I 128 UHu owuo>oquHE m.¢NoHH .«om EnH aoHquuo an .unn uaE > .EnH anHQ Hou Hov an .so xv m.-oHH o EnH an oaoHn x0 “H.-oHH o EnH ooun Uuo> .EnH aoHquuo an .aUnov \3 anHUva ouOE Eon EnH Hov squn UH. nNmHHI. o.HNoHH Uau wEnow aHow won .OEon Hou Hov squn UH I Euv vow Uuow .unn oEow .EnH aoHquuo an \3 EnH «u > so UH Han van uHo voa saan .onuu an nsuoanan \3 oaoa .n.ououn o gm .nuouu n.o~ouu_ o gm». .~.nuouu o .H xua xv \3 ans uo u stn Hov so vaa I x=m~.. voa saan n.nHouu uHo \3 EnH voa «usn uaE \3 EnH a~+ “EnH an :H+ Hov so E I, v.mHoHH_ ans auquouo Hov an I n.muosu_ wnoun aH Hm saan uHo 0U a3 \3 UHEouUw saan .Hov squn EIUH I Euv vow Uuow .Qan uoa .anH on oouu uo u > \3 o.uun ans voa oouu uov on .so nu nuoqu auv von uuon .xanuc s.nuouu n voa .uoa uov sw,uu. nuoHHI, nHoHH on n.~uouu anH uoa .voa “aUQov \3 oouH ouOE Eon .EnH ooun .usn “EnH Hov an .so E .nHoHHI, H.Huouu on s.ouoxs aouu unom voa saan _ un HHav u > \3 EnH UOE “m.oHoHH w am.H EnH voa H.HHoHH saan an HHsv u > “onuu nHuonnaw \3 oaonoH 0Eon Hov un .so UH I o.oooHHM .uo E Unow oEow «voa snan soIHn “EnH an Uau Hov soIHn UH I 129 so aIuH H.6MOHH. Oan Hov u UnE noHu . o.mnoHH Iouo \3 HM onuu .anoEoow oH n OUaH onuu .OEon Hov u an .so E I ownn o uvn uaa .n.wnouu .so ,w.wnouu n uso .uo» o ans xua on so xv xgw..~ ouoa .oaoa uov u Iaua vaa I wEnow auow “ans aosquuo xua gm. .nnouu o .u voa saan n3 0U uHo oH \3 noun voa so Han UOE “EnH uoHao un Iao H.mnoHH oouH Uau Eon Euv vow Uuow voUonnEoo voa UoE .Hov u .so EIUH _ I. ownn o anH aqua uo u . unouu o .uac aon uoHau unIaoI . .auoov x: Houxsw ouoa .uaa .anu onus aau uau .uov u .so aIuH «noqu EnH an , non voUonQEoo «voa svaoHo oEow “EnH oouH aaU > Hov u .so EIUH HanHI auv vow uuow .wanow aHow aouu xun n.onoHH . Iouo an UOE “wnoun aH voUonQEoo voa nan UOE Hov EIu .so EIUH . I usn uaa .nmoHH o xo “n.o~oHux:ms.o .n.s~oHHx=w~.Hc . .smouuxaw.v .snoHuxgm.Ho auv vow ouow . , van wEnow aHow an \3 wnoun voa UOE “av QOU an .o.o~oHH aH oouuaH voa saan n3 OU uHo «EnH oouH xnU un> Hov u .so vaE I, v.v~oHH voa oaHaoHHow wEnow xo aoHquuo an Hov u an I Unow wEnow aHow noHquuo an u . a: m.v~oHH .UEo van voa u n: OU uHo aoHuIsaan .voa .HanH Hov u .an .so E I uau ans anuo uov u sw aIuH .nnonuI. 130 auv vow uuow .anH.oous voa Hov u on .so a onoHHI so a .an n.onoHH auv vow uuow .voa Hov u .so xv I v.svoHH o =ms.~ .snonH w an .uau.oHoan aosa.aon. :m.~ anH voa .uHu owuo>oquua .xsm.ucu .xgw.v~ .anu . so a .xHa n.snoxu aoHquuo an aH sHHnHoonwo usn “EnH aan Hou Hov u .so xv I nan: ovaUnov \3 E00 won uo E “uan “voa aoHu IIun .so «.mvoHHl InUo :H QOU oan “noHuIHoHHHw “EnH anHa Hou Uau Hov .qu EIu EIUH .a3 I wEnow aHow van anvEon oEow oan “nvoHH III on o.~nouu anus anH aau aoau auoov \3 wav ouOE wEnow aHow «uo E Unow \3 voUonnEoo voa oH Hov E\3.u so EIUH nvoHHI, an u.nnoHH ownn a wav wEnow aHow \3 voUonnEoo voa u Hov u .so vaE a I an mHvoHH wEnow aHow an oHo no onuu \3 UOE :ms.H Hov u .so vaE I ownn an «.HvoHH o Hsuw .xua uo u xun xoan .am. .so xvcuouas Hov u .so vaa I n.H¢oHH noousc ans aosquuo xxn aw. Hov u xun . I II «.HnoHH_ xua uo u so as .xoan .gmn. .o xvououas Hov u so vaa I one .gm.u on :3 .xHa H.252U a: Eoo voa saan uHo OU a3 oH sHao >nn wn oEnw Hov u .so vaE I, . «mH aoHquuo «oUo @ Euv I . vow Uuow \3 “EnH so HHsv oaoa van wEnow aHow an n.snoHHm xua \3 anH xso Huavvvoa o.uun .anu ooun xau Hov u .so vaa _ w.ommHH aoH 0U voa Hov so vaE s.owwuu UnE ouo oEow .UOE Hov so UHIE I n.omouu. voa snan oa .aoHquuo ouOE Hov so xv I oaHvaaouuaw UnE ouo an \3 ooun voa saan m.omoHH_ “Uaowoun UnE ouo «waono oao .Hoo “voa OU UOE Hov so vaE I_ Hoo .ooun .aHowva Hov so vaE nmmHHI o.nwouu o .m .nmoHH o an asxa Hoo .uau o.vonH_ saan a: on use «.wwoxu I wmoxu .anu ounuosuo Hov squn vaa I_ - I H.nonH EnH aan snan soIHn xv . I HanoiM Hov aov .anu xau Hov an .un a I. EnH oHnUquo .HsUw m an sn voununoow anH u ooun > voa xuaooun Huav Hov xua .un 2 «onHI so n.~onH_ vuIHHo3 .u UnE HanH uo EnH anU “oaoa Hov .aun vaE I. m.~moHH. usn “EnH anHQ Hou Uau Hov so E I 0E0: Hov so E «moHHI n.HmoHH Eoo UEo saan .ooun .xoU wva saan .Hov soIHn vaE I m.omoHH. EnH anHQ snan soIHn xv I an .so E m.monH EnH sUHw Hov u . m.mvoHH saan HH:v voa n.nnouun .aou .voa uov u so uHIa I HEnH onuu .EnHvaoH “UOE Hov u so UHIE vooHHI an «mH «ownn @ HOUaH am “Eon so . o.nvoHH anHa “oUo HoHHnunnaoa “EnH sUHw anHa Hou anU Hov u. so xv I o.~voHH ans anuo xau un> uau Hov - u so aIuH A I n.~voHH uoa Hov u so ox I H.~voHH aoH won aoHquuo Hov u an I EnH sUHw Hov u so UHIE «voHHI . H.HvoHH ans sun anuo aau Hov u an .so xv I Houas xov u so 3. HnoHHI s.ovoHH ans sun Hov u so vaa I UnE so UH 0U E van UH aooBUon ono vanoHuo so E v.ovoHH sHEovanu HoHHnunmaoa oHUnnw > “Oan Hou Hov u IUH .so UH. I won noHquuo “uan uaE “EnH onuu “EnH sUHw Hov EIu anIHNo xv oooHHI voa oaHvasouuaw una ouo .Houas .voa saan voonaw suvvo uov u so uHIa o.omouu 133 an o.mhoHH voUonmEoo voa Hov u .so EIUH I . on v.23 A, anH anHo aau Hov u .so aqu In . un m.mooHH, Houau .voa so Huav u \3 voa Hov u .so aIuH IA ~.msoHHm oaoa Hov u so xv I n.¢soHH_ una aoquouo xHa .w~.n .uaa uaa > .EnH anHo aau Hov u xun .so xv I aoH ausquuo .uvn .xnsoxuvgn anH :3 m oou ouOE «wnoun UOE aH Eoo wEnow aHow an “oHo .uHo .an «.HooHH sHHnuoaoo an. Eoo voa saan n3 0U uHo “EnH UOE Hov u .so xv . I . ~.HsoHH ownn van gov w EnH Uau “amo.n 0Eon Hov u so EIUH I .aoucvoa uo aqu gwn. u \3 oaoa Hov u IIso xv n.osoHu :H voa n.ovoHH saan a3 OU uHo “anvEon “EnH “HoHHHw aH uonoHu nUo .Hov EIu so vaE I .n.nnouuvcms. anH voa “oou ua uoa ouoa “son. n.nvoHH voa snan 3 0U uHo oouuaH “EnH oouH Hou anU Hov u so xv .an I voUonmEoo voa .ooun anH .anu sun aon gu uou oaoa Hov u xua .so a svoHHI m.vvoHH_ HanH «UnE ouo “voa snan “voa “UoE Hov u so EIUH I aoHu ~.vvoHH Isaan .oUo HoHHnunaaoa “0an Eon “aoHIEnH oouH saan .Hov E.u so UH I 134 F.0moHH oaoa Hov u unIso a Eov Hov Au ownn ua wav van wnonaHUaoo n.vooHH Eon an wEnow aHow mo onus “UOE “voUonano voa Hov u unIso E I. Hoou saan .wanow aHow xun soIHn .an n.mnoHH aaU > \3 o.UHn ouOE uo aH EnH qun xv .EnH oouH saan .Hov u .squn xv I an Honau , _xHa noHuIsnan sn vosoHHOu o.vmoHH a wEnow aHow .aun .so , an aonU EnH un uxUE noHuIsaan UOE \3 HanH saan .Hov u IHn vaE mnoHHI uEn m.vooHH oEow uuo E van u o.UHn .EnH anHQ Uau xaU un> nUo .Hov EIU . so EIUH In H . So: 333 «.393 ., HOUaH van wEnow aHow un oEow \3 noHuIHoHHHw nUo E so EIUH I, now an “am. voa snan a3 0U uHo Unow uaE UEo snan a3 0U uHo \3 ooun XUE aoHquuo an van Ho vu \s anH Houau van w.~nosu o ans voa so Huvv n.~noHH voa \3 o.uun gm. anH so xv oaoa uo u .anx anHo uov u an .so xv I, . on 9233 EnH oouH Hov u .so EIUH I an H.onoHH Am.osoHHvam.H EnH UOE noHquuo an “EnH voa xnU Hov u .so EIUH I vaaon w Eoo Euv , vow Uuow “n.ssoHH soHon Eoo EnH an xnU “Eoo an n.osoHH EnH voUonnEoo voa so HHsv “EnH anHQ xnU un> Hov u .so vaE I an anu anuo aau Hov u .so aIuH nsoHHI n.5ooHH wEnow aHow \3 EnH UOE voa Hov u an .so E aH Uaowoua voa snan so . n.sooHH UH Han van UOE unn wEnow aHow Uau Uan 0an man Hov EIu an I, uan .xanH oouncuoa Hov u xHu nsza soouHI gm. unwnn . n.wooHHm aH voa “ownn ua uan “can svvnE “EnH oouH > Hov u so E I xua . on «.mooHHu ausuIHosHHw a van Ho voaouunuu uo u oH \3 Houas Hov .nuo aIu .so aInH _ I III s.nooHH voUonQEoo voa Uau Hov u so EIUH I, - n.nooxuw wEnow aHow «HHw oaHon HOUaH oH “Hoo “UOE Hov E an .so xv I Ho Hoo “noHuIsaan “HHw “ooun “UOE saan .Hov EIu .soIHn xmuw vooHHI, . v.nooHHH ownn ua aoao ouoa Hoo Unow Hov EIu soIHn vaE I . H.nooHH, EnH aan saan u soIHn xv . I“ Hnou snan “~.HooHH w EnH noHu xmn H.~ooHH Iusa u > “moo noHquuo “uan uaE “EnH oouH Hou Hov u .so Eva I_ so E _ onuu usuoa \3 anon on ans uau Hov u .squn xv nnoHuI «.sooHH, wouannuu NHuoa \3 OEon Hov u soIHn xv . I 136 oUo HoHHnunmaoa . \3 xUE uo E 0U u van voa snan aH noHu > aoHUoow usm .saan m.nHo~H anU aH snsvHE “voa usn van saan “EnH Uau > .Hov u so E I unn "EnH oouH Hov u an .so Et m.sHo~H , xs.suo~uvgw.~ anH n.sHo~H HanH “EnH noHquuo an oouH anU uaE \3 oaoa Hov . u an .so E I EnH onuu “HOUaH “UOE Hov u an .so E sHowHI n.mHoNH unn “EnH oouH Hov u an .so E I Huou snan saan .Hov u Iso E «HONHI o.HHoNH auoov \3 uoa awn anu Hov u an .so a I ans anuo saan u swusn xv Huoqu iso a. .803 uvn xnww aosquuo xun .anu onus on anuo uov u vaa .xHa I m.~°o~H onuu uHuoa \3 0an Hov EIu squn xv I «on an noun ans u van xun :n soIHn unwnn \3 aoo ans aoquouo xua .anH anuo can > saan .Hov u xx .xHa nooNHI III «.Hoouu onus uHuoa \3 oaoa Hov u squn E I soIHquH w . ooomu nunU uo E Unow aoH voa noHuIsnan soIHn “UOE snan .Hov EIu .squn E I 3Hn van H. wooHH w oaHaaHoon wnoun . as ans oxuu nan voa ox aoqusaan soIHn auau . w.noouu Unow uo E .EnH .voUonano .Euv vow Uuow .svsoHo Hov EIu soIHn xv I ¢.oNONH aoHquuo “uon “EnH Hov u an An.n~v~uccm.~ aun ans voa .xzwn..n aoo anH aoquouo xua \3 anH Hov u .so vaa _ ouonuI nUaov \3 aoHuIHov aun ouOE Eon QOU ua noHuIsaan noun “EnH Uau 0U 0E0: Hov u .so vaE nNoNHI n.mNoNH ouo aosquuo aau .anH nu xau Hov u so aIuH I m.muo~H uvn .anu Hov u xHa .so a I onuu nuuoaaaw \3 oaoa Hov u un .so on «nonuI H.nNONH aoquouo uov u xun I Hoo «m.-o~H w uoan u3H onuu Hu xuunw uosou onus > \s xau ans. ans xua \3 ans voa Hov u xun .so a nnonHI H.-o~H EnH anHQ Hov u so E I n.H~o~H so “ama. voa saan uHo \3 EnH voa “UOE Hov u so E . I Hoo “voa m.HnoNH wn van HanH vanoun Hu Eoo UEo snan uHo "HanH Hov u a: .so E I EnH voa HHnuo>o “aoHquuo van oouH uunw so n Hov u so E H~o~HI Hoo “voa m.o~o~H on van HanH vaaoun Hm Eoo UEo saan uHo “HanH Hov u a: .so E I . nuaw so m uo v “HanH “voa snan “UOE “voa Hov EIu so E owomHH;_ EnH aosquuo an cm. x: Houununoaoa ouo .s.~no~u m.Nv0NH u so unvoNH 0U asov EnH u aH Eoo usm vonno Hov .snan u soIHn xv anH aoquouo xun u.uno~u. saw. u oao \w EnH Uaouonoo ouOE \3 >nn wn oEnw Hov u so vaE I. EnH onuu UOE “wEnow aHow Hov U so vaE HvoNHI onus UOE Eon EnH . v.ovo~Hm “voa van EnH voa snan so UH HHav “unn “EnH oouH Hov u so vaE I .onuucanu uoa , «.ononu “ans. voa snan so UH Han oouuaH «onus NHuonnnw Hov u so vaE I . mnowH I m.sno~H voa Eon “onus NHuoanaw \3 0Eon Hou «m.mno~H _ _ InnoNH Eouu voa snan u van EnH un ooun HHav Hov EIu on .so UH anomHI :mm. EnH aaU Hov u an mnoNHI h.vnONH Hoo «H.vno~H o voa saan an “0an «QOU w so snan .Hov E so E .an . I, o.nno~H, Hoo “Oan “aoHuIsaan saan E so E I s.nnouH onus Hu saan snan .Hov u so E . I v.nnomH uon uaE “wEnow aHow Hov u an .so xv I n.ono~H on .so. n.nno~H o uaa .anu un van u a unauuwuv \3 anu anus saan .uov u IHn aIuH I s.o~o~H anu ooun uov u squn uH . I 139 EnH oEow aH Eoo usm u > “An.vmo~Hv=m. ..~.nwomuogw.u .xs.nmo~uczu .xo.Hwo~Ho=ws. n.nwo~H .xo.vwo~H..m~.u anH anow aHow .aoH .anH anHo uov .saan soIHn xv ‘ I onomu o xvoHomuu aan uuaw vouaauu , . “saNH.. v0: saan uHo u “wEnow aHow “QOU a so Hov so vaE omoNHI «.ononu o ouvunou voa s.ono~H oH .xnwn..n .x~.ono~u..~ anu aoquouo xua .anH uov xun .so xv I. ~.ovo~H w aoHUoow «.ovoNH_ usn “EnH aoH 0U voa “wEnow aHow \3 EnH Uau Hov an .so E I. unn > Hov so UHIE ovomHI n.nno~u. Euv vow Uuow “uoHoo un> UaoHHw “.voUonnEoovvoa Hov an .so xv I, «.onoNH m sUHwonov EuOUwVUOE “uan “voa “HOUaH Hov an .so xv , Ih m.svo~H. wEnow aHow “EnH oouH Hov an .so xv I . n.sno~H Uaon “onus “aH\3 EnH Hov so EIUH I aoH oEow waHquHE .Euv vow Uuow Hov so E ovoNHI. n.nno~u o ouaunou unusauw onuu .as\3 ans uov soIHn aIuH n.wno~u EnH uo u un oan .uo E oaHnonouQan EnH oEow EnH “oowwn musw so an «.mvowH .xo.wnonuo=mn. ..~.mnonsc=w~. anu aoquouo xun xov .un .so a I. . sUE . anqusaan .x=~H.vn anH aoquouo xun .stHnuoaoo an n.nno~H, EnH onuu aaUVHOUaH “EnH noHquuo an amH. \3 so snan .Hov .so vaE I. 140 :H aouu Iouo xHa .anu nxuoa o.nno~H .wanow aosquuo u, «.vuonx > «voUuOUaoo .aunU Euv vow Unow “wEnow aHow an Hov squn EIUH I onuwvnu anH aoquouo xHa .gmA van =w~..~ .anu Hov xHa .so a. I H.va~u voa .voa Hov an .so xv I Oan Hov an HvowHI ,. «.vvomu 0Uo wsoHHou “voa voUonmEoo Hov so EIUH I on u 633 an wEnow aHow usvoUonnEoovvoa “EnH Hov sso vaE I onuu usuoanaw \3 oaoa Hov unIso a. n.owvnu ~.owo~x on s.owo~u asov Houau “ansuIsaan .so nu Huavcvoa .anu uoa Hov uaIso vaa I n.nwv~x awn. van own. ans aosquuo xun .anu xun I . uan «Euv vow Uuow voa “EnH UOE «>nn anaU 0Eon won Hov an .so E mmomHI n.nmo~H aoHon oouuau voa v.vwo~u snan soIHn 0U so Han “onus NHuonnaw \3 0E0: Hov «n .so E I nuwmonu ans .anu uvn voa so as uov an .so xv I anH uov xua .un mnvnuI o.nmo~u anx voa Hov so on I 'IIIIIIII «.aooNH Hn noHu . an n.nso~H. Isaan .wEnow aHow .UOE Eon “EnH aan xnU un> Hov u .so vaE I EnH aoHu . Iouo an .amm..~ “usoNH ua UHu owuo>oquHE Hush vonno oEow “EnH voa oEow “EnH oouH Unn3oEow Hov EIu so vaE nsoNHI. . H.Noo~H voUuOUva van onum >nn EnH nan Hov u soIHn E I Hsonu o .saovmmmxxmmwaosmumsI- I I I n.Hso~H. aau .onuu nuuoanvw so .usonu :ouoa ans awn oaoa Hov u squn a I «.ooomH uo E Unow .sUHw .OEon Hou on .Hov EIu soIHn E I . s.ovo~H Euv vow Uuow oEow .EnH oouH Uau Hov u squn E I m.ovo~H. uo E Unow \3 0an Hou oUo .Hov u so E . I II n.ononu onus NHuoansw \3 oaon Hov EIu so EIUH I . v.mvo~H. ownn o anVEan u0an Hov u squn E . I ~.nno~HH Hnou saan Hn oEow “Euv vow Uuow xvoUonoEoo voa Hov u squn E I .v.svo~H, EnH anHa Hov u so xv I ownn o :mw. EnH m.vvo~H aoquouo xHa \3 .auv vow uuowvanu aoH vouuouaoo uov u unIso vaa . I_ 142 . on .xHa onuu nuuoanvw \3 oaoa Hov u .so xv _uoonuI u.voo~u ans auquouo xua .xgn on on. Hanan Hov u an .so a I w.onc~u. aoqusaan .anu Hov . u an .so xv I V on .an annouH onuu uHuoansw \3 0an Eon “unn “EnH oouH Hou Hov u .so xv I‘ anH Houau voa xau gm. .gwn. van . m.nno~H aw. .n.nno~u o uvn .voa .saan .anH us van xv Hov u so xv I. canonsm usn “EnH oouH Hov u an .so E I . II. Hnnno~H_ woovo vanoun UnE ouo an \3 am voa saan snan .Hov u as . I H00 .saan uann .uoa .Houas Hov aIu ,Iso xv nnvnuI EnH noHquuo Hov u an «nomHI . o.Hno~H EnH aan snan u soIHn xv I Eoo uuvaoa :3 .xHa ,H.oso~u Uno a3 \3 EnH «wEnow aHow “EnH oouH Uau xaU un> Hov u .so xv I_ ‘ «.osomu. EnH aan Uau . Hov u so vaE I. Iw.sso~H_ ans uoa Hov u so vaa I usn uaE > “H.moo~H w.shomH n anux axon ausquuo xua .anu anuo aau Hov u so xv .xun I 143 uan «UnE so E “wEnow aHow «EnH u > an Hov u .so vaa nounuI an v.n0H~H UOE nan «wEnow aHow onuu xvoUonnEoo voa Hov u .so vaE . I. an . unn «UnE so E «wEnow aHow “EnH u > Hov u .so vaE v.noH~H «.soH~H_ ownn w UOE “onus NHuon \3 0Eon “EnH am.H Hov u an .so xv I UHu owuo>oquHE ,an . .non ans xua aoquouo .anu oouu xau un> uau uov u .so aIuH nounuI. , usn uaa “.H.oocnuogw. .xH.woo~HV=u .xn.noo~H.:m~. on xv .an .aoo ausquuo an .anu anuo xau un> uau Hov u .so xv oounsI vaaon on auov \3 ans aoqunuo woo aIu a: woonuI aun xv .an o.moo~u now .w.~ ownn ua aosquuo an “ans anuo aau Hov u .so xv I, m.moo~H, auov vow Unow .anH anHo xau un> uau Hov u squn EIUH I Hoo “snan Hu onuu «Unow wEnow aHow “nanoH am :3 .an .o.voomH voa snan n3 0U uHo oH “UOE van HanH «aoHuIsaan snan u .so xv I o.Hoo~Hm oou n so .aoquouo Hov u xHa I EnH voa oEow “EnH onuu oEow w.Ho0NH. “Eoo EnH oaHUnunaow wEnow aHow “EnH oouH Uau Hov u an .so I I «.HooNH, non aoquouo .anu uoa Hov u an .so xv I 144 m.oOHNH EnH oHnUasuo “voa saan a3 0U uHo Hov u squn EIUH a3 .an v.oOH~H Hoo “HsUw “UEo Hno “ano “sam. 0U nsvHOUaH wH EIu .soIaun xv I . oounu o anH own. aoquouo an xo .xsnvanux Hov u sw UH ovHuxI . n.noH~H ownn a voa “HanH “aoHquuo “usn Hov u so xv .an I ans oHn van oaoa Hov u sw a anNHI s.soH~H Hu onuu van ems. voa snan a3 0U uHo “Uau HanH Hov u so E I III n.sounu aoquouo Hov u xun I , «.soHNH ans u > Hov u xun .so a I H00 .aoqusman uuo Houau .w.nou~u on a: a: EnH .uHo noHuIsaan UOE «vOHmH w EnH UOE aoHu ,.an .aun H.s0H~H Iouo an .uHo aoHuIsaan .HanH “usn “EnH UOE Hov u .so vaE I o.moH~H Hoo “voa saan n3 0U uHo “UOE Hov EIu so E . I II n.on~H 0E0: Hov u so E I H.moH~H aoquouo .anu u xun I auov vow ouow \3 “gm Hnwnn van =u oou au wav an .un xv sHHnHoomwo wEnow aHow “Euov vow Unow “voa “UOE Hov u .so vaE .moHNHI 145 o.oHHNH auov vow uuow Hov u squn a w.nuu~u uva .anH uau Hov u so vaa I w.v«u~u onuu wHuonnaw \3 oaon Hov .u so vaE I .w.~ unwna unAnsw aosquuo an .uan “non aoquouo an .anH anuo Hov aIu vaa .an nHHNHI mfivflm aHow \3 ans vouonoaoo voa «HunuI .oaoa =w.~+ xun I .vouonoaoo voa ua u .wanow aHow .uoa .m~.~+ I Hov u .squn xv nuHNHI wEnow aHow II sn voununoow ans onus > .uo o suuaosuw n.nuu~u xun w.nuu~x «:uaU wEnow aHow wav Hou an 0U o xv :H+ Hov u .squn xv . I H.nuu~u oaoa Hov u squa vaa I w.~HH~u EnH onuu «UOE Hov u squn vaE I , s.~HH~H onuu Hu snan “Hoo saan .Hov EIu squn vaE I wvHOE onum “HoHHnunaaoa “aoHquuo an - «.wHHNH .ownn o wEnow aHow «Eoo am. voa saan uHo “UOE Hov u so an vaE I Eoo UEo .voa saan a3 on uHo .xwvuoa onuwcwou .Hoo .uouau Hov aIu an wuunuI xanu xuncowna o xo sHuaouuw . .QOU o voa :H Uaowoua saan a3 0U uHo .usn Eoo H.oHH~H non aoo ans ausquuo xua .anu oouu xau un> uau Hov u xHa .so xv I 146 D.HMHNH usn sumo noHquuo «EnH aan Hov u so E .an n.n~H~H, Euov vow Uuow .UOE .EnH aaU Hov u so E. I m.w~H~H_ wonuu uHuoansw \3 0E0: Hov u so E I :Ha Una onuu smug >nn anau uo o sxuaouuw w.n~u~uI .aoquuso .xvovnuac noHuIsnan .wEnow aHow .onum .HanH .onuu Hu n.v~H~H uHo saan .auov vow uuow .voa n.n~u~uI .oou o xo Hov aIu xua .so xv I. HanH uvoa an snan uHo oH \3 oowwn ooun UnE aoHquuo an “UOE Hov EIu .so vaE vNHNHI , ownn II, I . a so “ano “H00 unoHuIsaan «UEo Hno an > HUUaH wH EIu a3 .an vawHI mm .an w.-H~H uaE awn. uHo voa saan “EnH aan xaU un> Uau Hov u .so xv I” :3 .an «.Huumu uvn .uoa Hov u .so xv I ownn o aoquouo a: ann s.o~H~H, xua cw.~ “non aoquouo xua .uva .anu anuo aau uov u .so xv I. o.nHH~H ans aau Hov u so xv IA w.oHH~H_ uon “UOE UnazoEow EnH Hov u squn vaE I an , voa on Han “wEnow aHow “EnH aaU Hov u .squn E sHHmHI_ 147 n.unu~H n so “ausuIsaan w.uvH~H “wnoun vonooaw nunn oEow “EnH ooun “EnH sUHw saan .Hov EIu so xv I «.onHNH OEon Hov EIu so E I . ~.owH~H. ouo ooun .o.nnuwu o ans suuw .anu Hov u xua .so a I_ n3 _ EnH “oUo HoHHnunana Hov EIu .an .so E nnHNHI. .\ o.an~H_ sUE sUHw aH voa vaw no vn qu E :3 .so UH ,I. ouo Iw.swu~H HoHHnunqaoa «unn «EnH ooun “xHanvEan “EnH oouH Hov EIu so vaE IN «.wnH~H_ xsmn. on oscuouau Hov u so ava I. uoHao «.vnHNH, wonuu NHuoansw \3 Oan .Hov u aoIso E I, uoHao , unlao . UnE unIao Haou snan Hn “voa nan .saan u .so EIHn mnHNHI Hnou UwOE Hno .saan u so EJHn vnHNHI .n.nnH~H. wanHo aaInHu «UEo oHno Hoou snan Hn wH .saan EIu unIs .un I saan so H.nnH~H aoHuInUo «HanH “EnH .Hov .qu E Iun E .a3 I. aoHuInUo “aoHuIsaan «HOUaH saan .nUo E a: Hso E nnHNHIM o.~nH~Hm ans anuo u soIHn xv . I, saan 148 «.oVHNH onuu uHuonnnw \3 oaoa Hov u squn vaE . ownn o anH aau squn 3 w Eon «nDHquUo “.an UnE onuu u .un o uvHanH nUo E .so UH .as. ovHNHI o.wnH~H, uvn Hov u squa vaa. I v.wnH~H_ onuu NHuonnnw \3 DEon Hov U squn vaE I H.mnH~H .sacanux .anu anuo an» > Hov u squa vaa . I onuu nuuoaavw \3 oaoa Hov u squa vaa wnsnuI . v.nnH~H, voa saan soIHn svaoHo van onuu NHuoannw \3 OEon snan .Hov u squn xv , I DUD HoHHnunnaoa aun .an , “nDHqusQ “wnoun UoE "EnH oouH “HDUaH snan .Hov DIE .a3 .so UH vamHI uaou saan w.nnH~H "DUD HoHHnunmaoa v «aDHqusn “HanH an o u saan .Hov DIE an .so UH I o.~nH~HM noHqusQ won munw aun aaU “svaw nUo DIE a3 .so UH I n.NvHNH_ DUD HoHHnunaaoa anHUva m “HDUaH “UOE oUo DIE :3 .so UH I w.ununuu oaoa Hov u so vaa I . b.H¢HNHU DUD HoHHnunmaoa sanE “EnH oouH sUHw van svaw nUo DIE a: .so UH I, 149 anu an v.Hnwuu anuo xau un> uau .gwn. aoquouo anI .oaoa sn+ Hov u .squn a I u.Hvu~H awn aosquuo .uva .anu anuo xau un> Hov u so xv .xua I ssnz EnH N Dan Hov u szE omHNHI Hoo .uao so s.wwH~H van voa wn aosuIsaan .xvu .sm.u on ovcuouau Hov aIu Iaua vaa I , so w.wwu~H uan «EnH oouH xnU un> Hov u Iaun vaE, I squn a w.st~H uuaouuw Hov u .soIaun xv I n.stNH :uaU wEnow aHow “EnH aan aaU > Hov u squn xv I n.nmu~u o I s.nmu~u noun UOE cm~.H van EnH aoHqusn aaU > “EnH anHa snan u soIHn xv I ans anuo saan u soIHn xv nwumxI_ s.HanH EnH ooun “ooun Hov u so vaE I. n.HmH~H_ EnH aan saan u soIHn xv I n.owH~H oaoa Hov u so a I. xanu,xun on non van EDU n so sHUnoHva noun voUuOUva mo ownn @ H van oou o oao anH ausquuo an xgmn.vn .u.wnH~u m.wnH~H. Io.nnunx aouu anH vouuouwsv .anH xau un> uau Hov u so a I, 150 . n.owHNH uuu unauoanua .anH non aoquouo Hov u so xv,.xun xun .so H.st~H .cw.o~ aoHquuo an .uva .anu anHo any > uau Hov u Iun.vaa I v.va~u anH uau on oaoa Hov u squn vaa I H.an~u aoquouo Hov u _xua I sun sw,>an on o.wwu~H o wanow so , aHow aun .voa gm. oou o ans uo a aoqunuo a: nuo aIu .un aIuH nounuI ununx o anu voa ua gm un a .so w.wnH~u ununU wEnow aHow Uau \3 voa soIHn u .aDHuIsaan snan u IHn vaE I ,. «.oounu aosquuo Hov u xun I wonuu uHuonnnw \3 Usn oEnw onU :N EOUUon «wonuu «.vaNH uo voa oaHvanquw wEnow aHow u > an \3 0Eon Hov u soIHn EIUH . I w.nnumu o anH ausuIsaan uoa gw.u .owna an .so v.an~u o anu aoquouo an .w~.H .anH anHo xau un> Hov aIu Iun vaa . I n.nnH~H EnH aan saan u so xv I n.~nu~u aoquouo Hov u xun. I an n.~wH~H u.~nu~u o anH .wn.u Hoo ansuIsaan .aoH anxo xau Hov aIu .so vaa I EnH anHa Uau xaU un> Hov u so E wvaHI 151 ownn an .sw ~.wsH~n ua wEnow aHow an van EnH.voa an \3 so can: Hov u vaE .un E I . H.ssHNH 0an 0U voUDnQEoo voa Hov u so xv I H.vsH~H ans onus aau .aoquHosHuw nuo u xun .a: I n.wsu~s o .u Houau voa .aosquuo aau .anu anus Hov u so xv .xHa nsunuI . «.msHuH unn “EnH oouH Uau Hov u soIao «n E I , H.osH~H o uoHnD v.vsH~H EnH aDHuIsnan soIHn am. «onus NHuonnEw \3 0an .Hov u soIao an E I uvn .anH auov vow ouow m.nsu~n .xua vaw aov Unow wuwnuu xvau .uo us Hanan ua xv .so w.nsH~H .w.n+ “ans anHo uau .u+ .anu uoa =u+ .aOqunuo uov .nuo aIu vauH .az , I “EnH u >vanHUva ouOE ANHuonnvawnoaaHUaoo ouOE .wav ouoa wEnow aHow sHao >nn oxHH Hov u an .so xv nsHuHI . s.HsH~H uau auau wanow aHow .xuauc voa .uoa Hov u xun .so xv I oHnwOE an o.osH~H .vason o wEnow aHow .xso aun un HHsvvvoa saan Hov .saan u .soIaun xv I an v.osH~H wEnow aHow sn voUnunQow .EnH aan aaU > Hov u .soIaun xv I , «.osunu una oun .aoquouo Hov u an I so xv Io.ovH~H osHmH .ovHNH a AanEan “EnH anHm aaU uau Hov u .squn E I 152 ownn a EnH. o.an~H aosuIsaan voa so uH .w. .onuu nuuoaavw \s oaoa Hov u squa vaa . . I on xv w .anH wEnow aHow Unow «aoHuIsaan voa “UOE Hov u .so vaE I uo a \3 Hanan oH uau Hov aIu so vaa wwunuI n.st~H uoa .voa Hov u squn vaa I . «.stuu uo a \3 Hanan oH oao Hov aIu so vaa I uoHno uoHnD «.vonH "cm.H 0U a: HDUaH \3 van voa ouOE Unn >nn oxHH .Hov u soIao vaE I o.~wunu o no aoIsHunuooowo .H.~wu~u uoHao «.oounx w am.H Unow uo E “onuu NHuonnEw \3 Dan .Hov u soIao vaE I I Hno n.HwH~H anH anuo gm. Hov u xv .un a I . voa .voa soIHn v .Hnunu can on Hoou soIHn aoau .s.owu~u on aaov on saan .Hov u xv .un a I , w.osH~H EunU Unow usm u \3 Dan Hov u so xv I on w .osumu EnH oouH anHuInUo nUo E .so UH .n3 I n.osunu new aoquouo xua .anu anuo aau Hov u an .so xv I an usn uaE “EnH anHm Hov u .so vaE oonHI 153 nUnov an .so «.voamH \3 oouH ouOE sHUnoHHw van anU “EnH anHE xnU un> Hov u Iun EIUH I v.no-H Dnuu NHuonnnw \3 0Eon Hov u squn EIUH I a: .un w.Ho-u HDUaH “EnH xnU un> oouH Hov .oUo EIu E .so.E I_ . unIoan I anu anHo can Hov u .so xv oowqu n.ooH~H o vavoa o wanow aHow ‘ w.ooH~H \3 EnH Uau Eon «ooHNH onon wEnow aHow uoaon Hov u an .so xv . I m.moH~H m.ooHNH In.wox~u o anu onus voa .anu anuo xau un> uov u xun .so xv I_ anH anuo saan u sonv swu~HI_ an H.NoHNH vanon o wEnow aHow aun \3 voa Hov u .so vaE I uan uaa on w.Hou~H “EnH voUonano u voa oEow “EnH anHa xaU un> Uau Hov u .so vaE I . «.ooHNH aosquuo uov u xun . I u.ooH~H ownn w Euov vow Uuow “EnH Uau 0U oaoa Hov u so vaE I , s.ow«~H Euov vow Uuow «voa oH “UOE Hov u so vaE I ownn so m.owH~H_ o ans aosquuo xun gm. van gm “ans anHo aau Hov u vaa .an I 154 m.HNNNH n.o-~u o n .w.o-~u o u xo .anH Hov aIv on .so I ownn o HDUaH «voasnan HHEv u \3 EnH oEow «EnH snan .Hov E soIHn UH oNN~HI vaw noHuInUw “EnH UnnzoEow «DUD ua HanH uu «Um D n: .so UH oHumHI o.nH-H anH Hov aIu quso uHIa I m.nH-H wEnow aHow “UOE Hov u so vaE I anH Hov u so vaa wHNNHI «.oHNNH voa saan uau saan .Hov u xua .so a I v.vH-H a wEnow aHow “EuaU usa oEow am.HH-H «ImHNNH a wEnow aHow van voa .EnH Uao oouH N .EnH anHQ saan u so xv , I N.OHNNH van ounnu o .Hucanux .xgn ou oacanu xau Hou oEow “anoun aH oouHVEoD EnH nDHquuo an “EnH Hov EIu an .so E oHNNHI Uaowoun voa Hn . nDHuIsnan «usn vonno «EnH onuu “wEnow aHow “UOE Hov u unIso vaE nomeI voUDnmEoD voa Hov u so EIUH sommHI w.vo~NH Dnuu NHuoanEw “voa “UOE Hov u soIHn vaE I s.mo-H unn “Euov vow Uuow “EnH UOE Hov u squn vaE I , n.vONNH aoqunuo xxgmn. .uo ucxouau woo a as .an I 155 s.HnNNH m.Hn-H w aoH on oH \3 UOE “wEnow aHow Hov u so UHva uaa .aoH .voa Hov u sonvIuH HnNNHI .N uoHao ,so uH Hnwnn as uoHao .xuo nouns uoa anH .w.u \3 anH .Hov aIu .so vaaw onnqu DUD w Euov vow uano Uuow “0Eon o>wanE aoaU unDHquUo “noHuIsnan nUo .saan EIu UH .an ownNHI an .un s.s-~u w.s~n~u a one HouxnunoIaoa “ans u oouu Hov u Iso vaa I v.6NNNH oaoa Hov u squn a .I m.sN~NH aoHuIsaan “voa aoH “UOE Hov u so UH ‘ . I H.v-~H o .sn van Havoanux .anH w.n-~u oouH ooun oEow «>nn 0U unHHEHw EnH oEow “EnH Hov u squn E I an aDHuInUo “wEnow aHow “UOE “aDHuIsaan saan .nUw E so UH .an muuuHI u.n-~u o aosuIsman ,I. o.n-~u «Euov vow Uuow uo unn woo «onus NHuoa \3 0Eon Hov u soIHn vaE I .so EnH oouH anU nUo .Hov EIu .un .so E vmmmHI v.n~NNH EnH anHa saan u so xv . I Iso a. w.--u n.--H o Augeanux “ans uov aIu .so on nu I v.HNNNH svaw “xaH .uo uvHanH “aDHuIsaan saan .oUo DIE so xv I 1‘56 «.onNNH sta .voa Hov aIu so uHIa . «.onnmu ans aosquuo.saw xua van onnmu n xo .xunoanux Hov aIu so uHIa I w.wn-H. s.nn-H a EnH aDHquuo an “EnH anHu snan u so xv I w.sn-H nUnov \3 EnH Eon aoH “wEnow aHow Hov u so UHIE , I n.sn-HW wnoun aH EnH UnnsoEow “UOE Hov u so E . I :w. on a: .xv .uo u Ho .w.wn-x a: .so s.nn-x .w.nn-H o anH Houau m .auoov \3 o awn ans nuo a nu .an I on n.vn-H uouau .voa Hov u .so vaa I w.wn-H. anH aoquouo xun \3 ans Hov u an .so xv I s.wn-H. ans oouu .voa on u > Hov u so uH I w.mn-H. :ms. Hnwnn aH wEnow aHow “EnH anHE snan u so xv I w.nn-H. nUaov \3 oouH Eon EnH anHa «H.nn-H o usn Hov u an .so E I. am.H Hnwnn aH EnH Eon «UaoH Uau “UoE Hov u IszE nnmmHIn w.~nnmuv EnH noHqusm “EnH anHm usu .Hov u so E I 157 o.omNNH, o .Hnoaon .v.om-H o an sHUaoHHw .o.on-H o UHu HnauoanHa .n.on-H o .Haaoaon .~.wn~nH an o .anaon .anH xaU :H H.nn-H o aoH .anH Hov u .unIso UH HmNNHI moU ua voa .snan .n.nn-H o usosooawo IsoIUH «.wnnnH noHuIsnan soIHn “onus NHuoannw \3 OEon Hou Hov u .squn UH I, now awn Una ouo xHa no wvomIManov _ o.wn-Hw \3 an ouoa awn .voa Hun Hvao saan u > .an Hov u soIHn UH I , n.nn-H. aoHuInUo xHa .oaoa saan .nUo a a: .an I. now. Hnwnn aH m.vv-H EnH sHUDaHUva H.vv-H w Euov vow Unow “EnH Uau Hov u so vaUH I. sunn uaE van UHu owuo>ou IoHa so anH ua van xHa o.UHn oU ouaUnou oxHH ova aoHuInUo uo E sn wnoun aH ooun EnH Uau n.nvNNH Eouu. w.~v-H o EnH no uoUDnunao aH ooanao EnH oUo .Hov u an .so E I Hu vaw aDHquUo .uan oH AIIownn . H ua ouEUnou oEow «EnH aDHquuo zoo n “EnH anHE qu .Hov u an .so UH «nNNHI . I Eoo EnH o.ov-H aoHquuo xHa .uvnaa .>an anaU xaU sHUaoHHw anH Hov u xHa .so UH I m.ov~~Hn uvn .anH Hov u xHa .so UH I H.ov~mH usn “Euov vow Unow “UOE Hov u so UHIE I EnH aaU NHuon an sn onuu Oan Hov u so UHIE ovNNHI v.on-H, .Hacaon .anH Hov aIu so UHIa I n.5wNNH aun .an EnH ooun “voa “UOE Hov U .so xv I uvn uaa .anH aaU aoHuInUo unuso w.nv-H «nUQov \3 oou ouOE Eon EOU @ voa van UOE “EnH qu .Hov EIu xv .an . I, nunU onuu NHuonnnw “w.no-H . , szon onuu nHuoanvw \3 oaoa HHUaa aUaov uoHao so xv n.ev-H \3 uoHHnEw van ooun won voa “UnE ao Haou snan .snan u .soIao E I onHw uo sn Uoooxo awuaoaHUva , n.Hv-H 0U uqu an a aoHuIHoHHHw so xv \3 voa nUo aIu an .so xv I an aun aoHuIHoHHHw ~.ov-HA uo a 0U u s: uo u awn. oU an voa soIHn xv nUo .saan aIu un .so xv , I, . an aun uo a 0U u \3 gnH. voa u so xv xan. voa Uao a: \3 ooU n anH oouH aw. saan u so xv owNNHI . EnH w.om-H aoHquuo an an. “ownn o EnH ooun :m. “EnH anHE saan u so xv I, an H .HmNNH ~.vm-H soHon wEnow aHow “voa u HUOE Hov u .so EIUH I uoHau ao s.ww-H wnoun aoHuIHoHHHw “voa “UOE .Hov u Iun .so.E I. uoHao ao m.mm-H , onuu NHuonnEw \3 “Uauvvoa DU OEon .Hov u Iun .so E . , I an N.nMNNH uo u \3 o.UHn EnH uo E “EnH anHQ xnU un> Hov EIu .so vaE I EnH an m.~mNNH oaHUnunaow wEnow aHow \3 EnH u voUonnEoo voa Hov u .so vaE I_ an «.HmNNH sonuuvwEnow aHow Unow \3 voUDnmEoo voa Hov u .so vaE . I. m.ohNNH UOE “Hs vovan noHuIsnan saan o uHo .an v.osNNH_ ownn ua uo E Unow “EnH anHm Hou anU Hov EIu so Eva I H.osNNHW w.ws-H soHon an voa awn oaoa Hov u so xv I anH anHo saan u soIHn xv nswnHI, DUD Hnwnn _ w Euov vow Uuow .HanH .wEnow aHow an .xEvvoa . .an H.ss~NH .oaoa so a gH .HanH .wanow an H.ss-H aHow an .xaovoa .an .w~.n .anH anHo aaU .w.~ Hov u .so vaa I v.msNNH_ EnH aan saan u soIHn xv I ownn ua xgw.c anH aoHu uoHao oaoU w.Hs~NH Iqu so E N oan oan «wonuu NHuoannw \3 0an .Hov u ao .so E I .uo u .so xv 0U a HovHOUaH :3 o.os~NH_ aoaU «EnH so E uo u \3 QOU w EnH aaU nDHuINUo qu E .so Eva . I. v.0sNNH, EnH anHa saan u soIHn xv I .aoHcvoa vu \3 wanow aHow aun an .un . n.onNNH aoaU 0an so xv 0U E aoaU oou ua Auoovaoa on Hov u .so vaE I an H.ovNNHm ownn ua EnH anU Eon «xuvvoa “UOE Hov u .so vaE I m.owNNH. oaoa Hov u an .so xv I H.mvNNH anH anHo xaU un> Uau Hov u an .so xv I_ 160 an xuavoaon .uvn .so UH .aa .N.owNNH xuo E 0U u aDHuInUo van uo u an o.UHn .EnH oouH Hov u .soJao E I o.owNNH wEnow aHow so xv \3 UOE Hov u so E I, w.wwNNHH anuvvoUDnano voa .UOE Hov .u so EIUH I ownn o anH xHa gws. «.wwumH .an uo a aoHuIHoHHHw .xzwn. 0U «H. uoHanH Hov aIu so vaa _ I, an anNNH ., wEnow aHow an \i UOE Hov u .so vaE I EnH anHm vuo Hov u so vaE N.ooNNH anH anHo saan u so xv szNHI H.nw~NH o .Haavaon \3 anH .oaoa Hov u ,Iso a anNHI . N. mwNNH 0U n. anNH on xv .an w.mnNNH Eouu oH UnaaoEow voa \3 auaU voa .uan .EnH UOE Hov u .so xv I anH an N.nw-H .onuu nHuoanvw \3 oaoa =m~.n uoHao oaoU N.anNH. “wEnow aHow .voa .UoE :v «EnH anHa aaU Uau am.N .Hov u aoIso vaE . I uoHao II oaoU w.~w~NH . anuvvoa voaoUUnHu 0U onuu NHuoanEw \3 oaoa .Hov u aoIso vaE I w.owNNH .n.owNNH . w wEnow aHow an \3 voUonQEoo voa 0U oan Hov u soIHn E HoNNHI n.ooNNH UEo snan “.vu .un .uo uvHDUaH oEow “Hoo snan .Hov E as .an I IImomm. «.uonNH Isaan “ownn ua wav Eon wEnow aHow oEow \3 0Eon saan u soIHn xv I, n.NonNH EnH anHa snan u soIHn xv , I w.HonNH_ wEnow aHow o xv \3 UoE How u. so vaE I_ s.OONNH ano gm. x: oaoa Hov u so vaa I m.oonNH onuu NHuonnaw «uan oEow “EnH anHa anU Uau Hov u aoIso E .I m.ooNNH Dnuu NHuoanaw \3 0Eon Hov u aoIso E I m.no-H 3Hn an nsmumo H.HsoNH EnH Eon «wEnow aHow \3 voUonano voa Uau «UOE Hov u E .so vaE I aHn uo a ~.mw-H >nn on a: .souun o.no-H anuVEnH “EnH v.Euov «Eoo wEnow aHow anoHuInUo Hov .on EIu xv .so xv . I a: .smuun v.noNNH Uau saan .Hoo .ono .gw. oU aacHouaH saan .Hov a xv .o xv I soIa. v.noNNH 0an Hov EIu .an .un E I anH anHo saan u soIHn xv IIInonuHI onuu nHuoanvw \3 uoHao an .so «.HoNNH Oan cm.H Huan .Hnou .UOE :oH “EnH anHo Uau an .Hov u Iao vaE I an .so UH .as. H.ooNNH uan “EnH oouH 0U onuu NHuonnaw \3 0an Hov u .soIao E I 162 anNHI EnH oouH oaHUnunnow wEnow aHow u Hov u so I ¢.NHnNH EnH anHa saan u soIHn xv . I s.HHnNH_ wEnow aHow Unow \3 voa oH UOE Hov u so vaE I, smumonvI w.oHnNH, onus NHuoanaw “EnH ooun van voa UOE Hov u E .so vaE I ,. b.00an ownn o anH aoHquuo xHa .mn. .oaoa Hov u an .so xv I nDHu ¢.QONNH_ IHDHHHw “oouuaH wEnow aHow an “UEo nDHuIsnan nUo .saan EIu an .so xv I H.oonNH anH anHo aaU Hov u so vaa I n.son~H n aHowva .vu .anH Uau Hov u so vaa. onNHI H.non~H o anH on o u awn. .anH vuo oU oaoa Hov u an .so xv sonNHI. EnH nDHuIHoHHHw a3 .an . vu uo a van on uo u o.UHn .anH anHo xaU un> Hov aIu .squn 3 nonNHI .Hoou saanc=m~.H an «.wonNH 0U as HOUaH uo u xHa 0U o xv .aoHuIHoHHHw Hov .nUo aIu s.o UH .a3 I_ so o.voNNH a anvEan noHuInUo “EnH aan Uau qu .Hov EIu E .squn E monNHI H.vONNH, EnH aan snan u soIHn xv I, ownn van QOU w EnH IIw.nonNH aaU soIao E «onus Enow aHow xvoUonQEoo voa UOE Hov u so vaE I 163 H.0flnNH non aoHquuo anH aaU oouH Hov an .so xv . n.wNnNH_ EnH anHE snan soIHn E I. o.anNH wEnow waHow \3 EnH anU oouH Hov so vaE I. o.UNnNH. EnH anU > aDHqusn “EnH anHa saan soIHn xv I , . o.oNnNH Dnuu NHuoanaw \3 voUonano voa Uau Hov squn E I an . vuIHHoa oU vu .aoHuIHoHHHw nUo .so UH .as. ounnHI voUDnmEoo voa _ s.oHnNHI .aHn so \3 aoHquuo an =w~.+ .anaoH squn s.oHnNH aH sH oU on HanH nw.+ .anH aaU oouH =m.~ + Hov xv .an I, anH anHo saan soIHn xv oHanI H.vHNNH w.mHnNH 3Hn wEnow aHow \3 voUDnEEoo voa Hov so vaE I n.mHNNH sUE aDHuIHDHHHw uo E samN.H 0U a: .uo uvHanH Hov .nUo so vaE I s.anNH ownn @ amN. EnH aoHquuo an “EnH uau 0U oaoa Hov so vaE I, EDUUon aH wEnow aHow oa xvoUonano squn . m.anNH. voa nnUaov o wEnow aHow \3 ooun .EnH oouH anU Hov xv .so xv I ‘ n.4HnNH_ wEnow aHow \3 voa Hov so xv I“ 164 on .ufifl HCE «EMA UOE H06 u .%D Xfilfl OvnNHl ownn a :mN. voa an M \3 EnH aoHu .v.onnNH Iouo an .o.nnn~H o =m~.H anH uo a .anH anHo saan u so xv I . HDUEH “N.vnnNH 3Hn wEnow aHow \3 «voUDnano voa oH “UOE Hov u so vaE wnnNHI an .n.nnn~H o xuoUwvHov . _ voa Uao van wEnow aHow \3 .Uau .EvvoUonano voa Hov u so vaE vNNNHI, N.NnnNH_ oaoa 0U voUonmEoo voa Hov u so vaE . I H.Hnn~H_ xvoonHuwHE annnouavaDHquuo EnH Hov EIu so xv .an I EnH aan snan u IsoIHn xv HnnNHI an an a: .un w.onn~H aH Hs snan vovan oH \3 Ho oH > \3 HDUaH “Hoo Hov DIE .so vaE I. wwov _ anH on :H+ .uvn an =n+ .xstnvwouvUnou wwov an n.vnnNH EnH un cm.H+ “wEnow aHow wav am.+ “Oan :N+ Hov EIu .un .so E I. . o.oNnNHm auHquuo Hov u xHa , I I an w.oNnNH an wEnow aHow \3 voUDnano voa E Uau Hov u .so vaE I. v.oNNNH, 3Hn so ownn w :H .Hov aoHquuo uEnH Hov u an .so xv I“ I N.wNnNHH anH anHo saan u soIHn xv . I. rant .6 IIIII ad \3 EIH any cI IIIIK, ECU 50: IN. 90AM“ 0 saw—“H “wagon“ 165 can n.a¢n~x ownn u and gap. nun xv x: xxx xxaov soquouo Hov xv .xxn . I . oncun U and auoumv uvsamaom Hov xv .xxn _mvnuxI; IINoIcua v.ocn~x. “on noqumao xxn “xxcvvavxx a “aux cvxa an» Hov xv .xxn I muIcun «.oennx, .u >ono “ovum an axe spam “Hope“ 0» uos Hov xv .xxn IA mwncun acaquuo “oao: on and vmuovneou v0: 050m Hov xv .xun ovnnul . ~.pvn~x_ Eva cvaa scan soIHn xv .. If xxn x.m¢n~x_ «on aux soquouo xxn “sax cvxa Hov .so vaa I xxn muvvnmx mason :Hom \3 kuovaeoo v0: Hov .so vaa I. . xxx v.v¢n~x mmvn w and :OwHIouo xxn :m. \3 kuovmfioo v0: Hov .so vaa I «.ccnmxu and Ham o» 050: Hov so vaE II «om noquouo xxn “voa xov xv xv .xxn nenNHI_ «.mvnmx ownn «woe xoquouo xxn “and cvxa xx» uv> ucu Hov xv xv .xxn I noquwxcv xxav «m.oenmx v =m~.x .n.oen~H v , ems. xavx vauovmsoo v0: u.ua \3 Eva ucu ou 0E0: Hov so xv .xaa anmaI EQH CQHQK sZCQK >0 Ht\ Hausa use xa:.uou a van uxo u van «was a: use no woman :u on \3 v0: ucu «zoflustcv sncv u soIan xv mmnnnI .820 so a x633 mavmm :Hom “v0: “#05 .Hov u .soIao xv . I aux cvxm ascv u mu.xv omnNHI vason w mavum :Hom \3 aux any > m.mmn~HI “damn an \3 oao: =m~.~+ xxn «.mmnnx “Man .vcaon w macaw snow \3 and can > :m.H+ Hov u .so vaa I .aun «.mmnnx :mwauun :« uos “xgm..aouuon vcv go» o avx an» Hov u xv .xxn I can _ oao: Hov u xv .xxn nmnwa Nu v.vmn- ownn w x0 “yap an \3 050: Hov u Inna vaE I 0mvn w «.vnnmu :mw. and noqumuo xxa “aux xnu uv> any on oao: Hov u an xv I ownn w Eva nun xv van and .qu mm noqusscv no a nun» up.nmn~x o» vu Huxxxm am a uvom vcv .u an .av Huang avg» um.nmnnx 0» aux ucu cu oao: no u Hov aIu .so vaa vmnaxI :m.x «om noquouo xxn vmuovnsoo av” so a .xxn. .x.nmn~H can > van no» u: nan «omuucw Eva omufi \3 050: Hov u .so xv _ I xxn m.~mn~x aux uxu noquauo xxn an» aom “xxnvavxx “svx Hov u .aun vaa I can «.Hmnmx «on son uxu xoquouo xxn “and an» > Hov u vaa .xxn I ”.33“ Eva cva sncv u so xv . I g Oman has «in End :2» “an... .un Hawk 6I~n CDVOECC Wax...“ .<1\ 167 uonO so v.own~a «.ovnmx taxoa ovuu uxuoxnau \3 oao: eon oao: .xov u .so vaux I vasouv no a x: m.pvn~x aoxma Houcx u.vx "vegan snag a mavmm :Hou vcv so a “ovum Hm sncv vuo> \3 Eva an «.ownua so xv am «no a uvou “nequsscv “Ava oavxoucw vuo .Hov HIM .so vaI I . an «.sonwa vo: ox ou u ucu Hov u .so vaa I, no: “o.won~H 30x03 mevwm :Hom xxn “v0: Hov u xnn .wo xv sonqu mmvn v xo “emu. xxa «.vvnuxm ownn o soflquuo xxn “nan “Eva own“ an» > 0» can Hov u .so vaa . II 1N0 h waHIouo “Man ovum “Eva own“ “van “voa Hov u vaI .xnn wonNHI o.mvn~a w x0 human w and 050: :m.H “Afinvevax xxn .aun s.mmn~a «Hocv 30H “wan nun soquouo xxn “Eva cvua an» > Hov u I .so a I xxn .aun ~.mvn~x Man uaE .an .ufivom :Hom \3 Eva kuovmaoo v0: Hov u a .so a . I, van no uuox .xavx ownn no Ho vuvmmvvxn sacv xxn .aun v.vvn~x \3 skuIouo xxn \3 #06 away “xfinvavxx oxocv 30x Hov u a .so I I xnn .aun new Eva uwu nequouo xxa \3 :2» Eva cvxa Hov u I .so I commaI m.va~H o.nvnmah @ ~00 vcv Hausa 0:0 ocficfivucoo “Eva cvaa scam u so xv I. uoHno mwlvaa , Houcfi .Aomufivvo: voa u .Hov u .soIao xv HonNHI =mu.v soIHn xv o.mmn~x «mun Han van and as» name an damn oIHn AunVOEoz sncv .aov u .svlun xv I kin «AEMGU 60m qumvErwn uCE ll‘ «on son nunnIono xnn “aux cvno nov u so xv opnnnI I n.05nufi Eva cvxn scan u so xv .I nodno co m .252 ooun o ava.u 503 qumm :Hom co xv \3 v0: u .Hov u .so vaa I . an ad w.monma Aavvo: uvom van 0» 080: Hov u .so vaa I go» o avn can ~.mon~n no u \i no a sHanocmo vn sownIHOanm “Hausa u Hov aIu xan .so xv I 050: Hov u I so vaa monNAI , an and Guam Hov u .un .so xv w.von~H Nw «.vonma uom sonnIono “nun “nos n nov u vaun .xxn I 90» w Eva neano m.nonNH so vcv no a an :OnnInuo “ovnu unnonnsm \3 060: .Hov aIu soIao a I v.nanH xofinIono xnn «ma “Eva cvaa sncv n so xv I nonnu xnn .cw o.non~n van :2» ownn .nov u .uo vaa I nonxu xnn q.m, m.non~n 902 “v0: omnfi a O» u .aov u .so vaa , I xxn 0 65.: Eva cvaa Hov u .so vaI I nexnu an .nm _H.connd nan “xenov vmm uncovevn nos .nov u .so vaux I 169 :nn Inn a .xnn «.monnn may n: nan “woo nownIono xan “Eva can > Hov u .so xv L an: Inn a .xxn «.monwn Hanan “ovnu an scam nHo “voa Hov u .so xv I o.von~nw 020: Hov u xanIcnn xv I . v.eon~n_ oao: Hov u so vaa II, oao: nov u Nm vaa conwnI noucn “nu II, , no a \3 xovnu unu>vn=n Eva an wco “Hausa oEow m.nwnun \3 xnn vn sonnInonnnm no a van on no u o.unv nov aIn nn xv .xnn I ”on sonnIono quna v.~on~n W xan “nan “nunmv \3 ownn Eon cvaa .va as» > Hov u .so vaa I, o.von~n o so “v.0onmn v gm mavmm III n.~vn~n , aHow uvmaovaaoo v0: ox o» a ownn new on 050: Hov u .so vaa I, m.von~n, and can > uvom \3 .vn cunnIHoanm nuo a xxn I an n.0wnNH vcaon w mavwm :Hom uvom \3 Eva v0: Hov u .so va3 I an .xnn , vn non xgm o» gov noucn nov n .so vaa . oonmnI mmvn , w mason :Hom any > cmnu “mevmm :Hom 0: con» xan w.oon~a_ vnoonma 0» :30v xan mfimom aHow \3 Avn omnfivvo: Hov u .so xvlfl I ovnu unnonnaw \3 soIao xv 050: :m.v “no: :«+ “no xv .nvn .aun can > =n+ «awn £3 vn IOanInuo \3 can and ownn.:m~.v+ “Hawn an uuo :3 .so non oao: xo : can.~+ “Anavavnx wnoun son =m~.n+ .nonso a .na .xnn “no: xnn sm.n+ “ovnn unnoxnnu \3 oao: =~+ .nov aIn .co xv . von~nI . . n.von~H ownn w and Ivan u on voa :svaoHo: Hov u ya .so I I o.non~n no n van a “awn n > nno .Hov aIn nn an .xnn I .INo «.aonmn no I uvom “Ham .uHIonum vuo .Hov IIu Inn I .xxn I nnm “non moo .voa nov n nn nonunI umvao unu :n “Amvco w.~onma voucnoa .Ivocncnxvso mason :Hom can \3 v0: Hov u so I I n.~on~H Iva Ivan sncv u so xv I no I \3 an ovnu unm> Iva no u “no an m.oonnu a van no n o.nnv “v.oon~n aonmn xomnn .avnoncn nno .nov aIn .so van I II nn ¢.ovn~n evn nan on oao: nov n .so vas I I, nn .xnn H.oon~n «an acnnIono an «msvmm :Hom “v0: voa can > Hov u .so vaI I mmvn w Iva Ivan v.oon~a Ion Iva no anon vouovmaoo Aunnon vmucmnnovvo: Hov u so vaI I an m.oon~a mvam caom "Houcn “v0: Hov u .so vaI . I memm 930% NH “5.560: H00 u EXCUfl bmnfldl 171 nnm> m.vo¢~n . nan oao: no n nn =m.n swan gm. son xnn no a nov aIn nn .xnn I no I anon \3 no u «Hov wvam unmnn voa an «.vovwn an Dnnu saan nHO «:m.v Iouuoa OIoa «mmnn w voa uuo .Hov IIu so vaI I Iuov vmm unom “30Hon mInwm aaom . o.mov~a 0: n.on van n.mov~n v canon snow \3 n “voa nos nov n xnnIcnn xv I Ina annn Iono an :m.n >nn yuan owns 9 x0 «wmnn na I00 HIOI Houaq “2H oao 30x03 Houan ann v.vovmn w . H.mov~H eon sunnIono xnn can. “nan nae “evn nan on oao: nov n xnnIcnn xv I mo xv o.no¢~n Ioo onOI nan .uuxv noHoo sHao >nn mn mInm Hov u .ann .xan I ¢.nov~n Annvavnx “avn :vna nov n so xv I an: Inn cvno nan on oao: nov n .so vaa AnovwnI >na noon sonnIono xnn can .omvn o xnn m.nov~n x0 uvn ao«nIHo«H«m no I van no u o.an .InH aau Hov u .ana .so I I unI nan Hanan vn \3 mmnn w no I Ion umInmm xxn n.nov~n axon xan anon “u voa saan nHo omnuan “uOI Hov u .ann .so I . I Anny xnn n.ooe~n Ion N name Ibo Ina aonnIono mwu aau xan “Ina Hov u .ann .so I I v.mom~nI~.mom~n Bonn avn . saan n so vaI oonnnI I an “vuo n: Anavavnx .aun cvno nofim H06 flHOl h. D 3 HQ .an oIGGNNH O N x g XVIII II mavom cnom \3 Inn vo: n v o.onv~n w Ada: Ion uvo no I mIomvsmo. van an v.nnv~H no» o xInnv vmn unomvzmo. Inn uOI “Inn aau van Hov u .so.vaI I nonxo nunnvnn onnu unnoaaam \3 OIoa .aov u ao .so I I . o.nav~n nan sonnInxcv “Hanan n nvnnau .nonnInonnnm «no a xna .uo xv I wmnn na o.oav~n Ina no I Ion van Ina voa n.u~ aau > mac \3 OIoa Hov u so I I H.vuv~n Inn anaa uau > Hov u so xv I nInuu axon xan mav \3 voa u > :mo.+ IINo vaI “nonnIsncv .noucn :m.~+ “oIna xv oao: =mn.~+ ‘xnn .so «Innx .nnn .onnm .uOI cm+ “qun xv OIoa :m.~+ Hov u Ian vaI nnvnnI «.onqun a sun can nan =~ \3 oao: nov n :nn vas nneunI noHao _ qum «aonnIsaan Hasv umInmm aHow aau unom \3 voa I on n nonznnauo um.oov~n w :mo.v .m.mov~n xnn u v :m. xmcv nonvmavmm exam \3 n nos “nan nov n .so vaa onvmnI m.mov~n voa uam ou OIoa Hov u an I I, wmnn van no» a Ina sunnIono xnn Imp. “ownncn non no “vnnsm nonn «.aocnn, Inonnnu no a snnvnacmo .15 on nononcn on oao: nov eIn xnn .xo xv . I mInmm aHow an xv .xan c.oov~a_ nos vo: n.~.no¢~n a gm~.~ \3 avn nan on oao: Hov n .so vaa I noHao ao .un m HOI umInmm aHow \3 voa u .aov u xv .an sovNuI 173 v.nnw~n voa nan > «HOI aov u so I m.anv~a Ina avanIsaan mIom “ouo oona sauaoaam \3 Ina aov u an .so I I aouaa .zmo. xan a.anv~a on n. voa acanIsaan an on so ua mIom \3 #0I aov .u .so vaI . I Ibo Ina xan acanIono «aua “Ina voa nIom “Ina aov n xaa .so xv anvNaI mnmnn ananIsaan _ J OIoa van Ina n xv amnsuon ouo amaannnaIaoa “Ina aov u so xv onvnaI avanIsaan Iona .Ina .. aau > ounuaa \3 van Iuov vmm nuom vouonQIoo voa saan u soIan vaI onvnaI o.o~¢~a v.m~v~n a non no a noncn =m~.n navn cvno nov .xzcv n no vaa . I >nn m~.o mn mInm :m.w+ “aamn nn an \3 xsvnoannsa nnIso no n =m.¢+ “unvvna aa Ina no u :m.a .uIU aoanIsaan .qu no I \3 no n xvn on on 5. Hanan sm~.o+ “son no a van so nn a .xnn no n o.unv :«+ “no a .vn on vnnsm .nonnInonnnm uno..aov aIn .so xv muvmnI Ina no u van no I o.uan Ion an anmna “Ina anaa saan n so xv nuvnaI a.o~v~a u > Ina uao “oona “wav awn mInmm aaom saan u so xv I Ina anaa saan u so xv ouvmaI anaIxaa o.oav~a u > Ina vac “ownn “wav awn mInmm aaom aov n .so xv I v.oav~a Ina onna xv aau > oonuaa \3 OIoa saan u soIan vaI I 174 aouaa “avanIono xan nouano aa Ina :a «ana van uOI Ion «Ina pan aov u nnIso na onvNaI nnIso. vevnvna xoanIono «Annvcma passage» “Iva aov n on .xaa I m.nnv~a oao: aov n nnIno an I n.nnv~a unaoaa 3nu anmnn aa ama «Ina omna aov u so I nxan I o.mnv~a oao: aov n naIso an I «.mnvwa xaa ananInuo “voa naI > “OIoa aov .nuo I xan I n.mnv~a oao: aov n nnIno an I ma a.mnv~a Ina omna una3onm aov u .so uaII I . .nnvevax xan o.vnv~n “aunwv \3 Auoavnan «naI Ion “aanIOaI “nan “Ina aov u .so vaI I .anvInax “Ina ao mIom “Ina ownn mIom “voa saan naI ao. n.nnv~a \3 AomnavIna Ion u>an Iona unI no uoxooa \3 MOI aov u .so uaII I a.~nv~a acanInuo .aoanIsaan .aUanIono IIu xan I ownn o Ina oan u > “AUOI unnamIomVOIoa awn aov u onun I «nonaI.1 o.anv~a Ina aov u so I I Innv vow anon “xau cm. nnnn xaa ananIono xaa «voa saan vaan acanIsaan «UOI saan u .so IIua ovvnaI. n.ovv~a Ina acanIono xan > «Ina anan saan u soIan xv I o.nvv~a xaaavInax van ouo aoaannnaaoa aov IIu soIHn vaII I. avax no mncnx “ouo xaanNo m.mec~n w Ina vaunoann» “Ina acanIono u v \3 Ina u > aov u xv .so ya I van I «No quoon Ina “x0 “auamv \I own 0n0I Ion Ina uOI I .unIso o.vvv~a una30Ion “Iuov voa anon «nan “Ina owna «nuanOaI aov u ya .so ya I , , v.vvvna abanInuo “acanIsaan “OIoa saan .Nuo I xan . I Ina so ya OIoa \3 o.uan .vuo amaannnaaoa III ".vvv~a nun x: son soanInuo no a nonnIxncv xnn can Inca aIn xnn .uo an I van Ina .oon unOI Ion Ina owna > uOI aov u WWIIaII vvvwaI ownn I! I m.nvv~a w x0 “Ana acanIsaanvaoa “auuaa “aoanIsaan “uOI saan u so I I noucn nn3 “nonnIono nov n xan nawav nvemnI xan .smev ~.~¢q~n nos “noncn “con aov n .nnIao an I uOI van Ina omna Ion “mwnaunwu umnv .nmnn sxaa xau xa vaaonn uqu man svaw aov .nuo IIu unIso ua avvmaI va cano onm «aoo “Ina avan Iono xan gm. “aoavn vcv one~n o Iva ovn once v.on¢~n Ion.uaoaaa “aoa “gm. on In Ioo voa “avanIsaan aov .saan I a: .xan I . nIoom . N.nmv~a .vuo aoaannnaaoa oaon \3 .aavInax nan «Ina aov IIu squa I I nmav oIom nmuun aa vounanon vII II anvam a: a0 xov .xan n.~mv~a xnn gm». vvnv xnn vvo «gunnIsscv “Agnv nun “nos aov n .uo aIua I «man a no “nonnIono aov n xna .uo xv uncunI . w.amv~a Ina a3 avanIsaan van xan u > nIom OIoa Ion Ina aov IIu squa I I naI unsm n.amv~a «nunnao oaasann>o Iunv Ina :m~.a on a: aouaa aov u soIHn 9a . I «.amvma 6 Eva Imam aov u so xvla I 7 1 v.cm¢~n OIoa aov u so xv I Ina no I mIom «.omvma \3 xv vIn oon mnOI Ion awa “Ina omna naI van > aov u so IIua I w.ovv~a Ina n > nIom Ina u “aoanIono aov n xaax I an n.ovvma Ina oona “an onnn acanIsaan “uOI “aonaa aov .saan I .so IIua I onnu au saan .voa saan “onnn aoao .vaan aov .saan u so ua ovaaI m.ovv~a IonnInno “xgmn. on on novnonca nno a no vaa I «.ovvna acanInuo “OIoa non .Ina uau >va0anIsaan saan .Nuo I xan I 177 n.avv~a wwov “noncn aov .nno aIn soInn an I n.00vma Ina omna “avanIsaan “IOI saan I soIHn vaI I I n.ovc~a aoanInuo “voa saan nao van un «Inn \3 mnI «no .I soIHn vaI I aoanInuo m.mmv~a “o.mmv~a w Inax \3 Ina «naI Ion “OIoa .mnI mnOI aov IIu so vaI I . m.mmv~a IO N uxaaavInax “ana oa “man “Ina avanIono “Ina aov n xaa .so I I amna w x0 “xaaavInax “auauv \3 vnoaaoaona onOI n.xv Ion Ina anaa nan aov u so I omvNaI aoo “Iuov n.0mvma vnn vnou “an onnu qu acanIsaan “aouaa “uOI aov u soIHn vaI . I ‘ so an .xaa o.mm¢~n mam “Ina v0nno3a30v “Ina “nan "auuaa aov u .so xv _ I o.mmv~a Ina anan aau > nan aov u so I I nan “yawn onn unau Ina ownn “xaaavInax “Ina aov u xan .so ya . mmvNaI xan on so xv Ion vno unau nmnn OIoa awn aauaa aunwv \3 van Ion “mnmnn aoanIono onm w.vmv~a “Iunv vuo vnon .voa saan vaan «a \3 Ina naI aov IIn xaa .so I I .I m.nmvna Ina anan aov u xv .so I I m.nmv~a aumnv \3 OIoa Ion Ina anan aov u xan .so I I 178 s.nm¢~n .ncvvavax “aov Iva nonnIono xnn I v.~o¢~n “nan nan “so an van soInn an .xan o.nnv .aun aov n soInn an . I s.oso~a nos nan aov n soInn an I «.osoun xuaoooov Inoum nanvnsa no u «aouaa aov n soIHn ua I . I n.osv~n Ina anan saan u soIao xv I noncn «Annvvoc scam \3 awn scan .aov oIa swung an ~s¢~nI aunov,\3 aao Iov Ion aoo “no onOI oIom vmnano n.oov~a on .xsn =m~.n.ao on > \3 noncn «nus nunnIsncv scan oIa xan I wvmm \3 sawnoaQIoo an onnu ouo na “ovoo avanIsaan no I \3 vmxaI Ion n.onv~a snoov \3 an scan nao .xnn Inn. on asvovnn .mva aov n soInn an I, v.ovc~nw an on a: .noncn aov n so a I «.ovvnn, nos aov n nn .so I. I, won aam no onwnn ~ “avanIsaIn “ama no voa uau aov u so.I . mvaaIM o.vcv~aw m.vwv~a w uoI onOI unanoa aoa Ion .Ina aov u so I I. «.vveua, nsn «n.mov~a w AanvInax “Ina anan saan u soIao xv I n.av¢~av nan aov .nno eIn soInn on I ooun v nonnIono x3 :2. \3 vo: on > on 28.. aov n soInn .— 222...; . moIcnn v.oo¢~a _ «mu soanIono xan “Iva cvno aov n xv .xan I ".oovmn Ina anao saan u so vaI I aoo>aao nOaao .uo a.snv~a mInoo aaom \3 Ina aau > oona .aov u Iso vaI I «.vovun xvoaxooom xnnvoaox “vn nonnInuaanm nno a xan .nn a II m.vo¢~n unI >nn \3 an Dona unw> “OIoa aov u an I I x=~ nan an vn n.vov~n nvaonca nn “.vvaxooau xanvoeon nvn nonnIaonanm nuo a xan .nn a I nnmoemn oao: aov n nn a . I Anvumvn o no asIonn “Anvvoc ~.mov~n oonnca vcv nan sonnstca nvn nonnIaonnnm nno aIn xnn .so xv I o.¢oq~n Eva song as» nan aov n cnn .so xv I xnvumvn o no ovIonn “Anvvoc v.voq~n ounncn van oao nonnstcv “vn nonnInonanm nno aIn xan .so xv I van avmvn oan nnsm xo one: "ownn v vcv .n.em¢~n xnn m.¢oq~n ,o .uo» a nun nonnIono mnn xnn gmN. n “oao: aov n .cnn vaa I v.no¢~a Ina Inao saan n xan .so I , I nInon aaon unIIna o.mov~a anon .aouaa n .vn ou vnnon .a0anIoaunna0a0aan ouo I .so xv I nnnn o a.vov~a Ina van van ana nu Ion qu saan \3 acanIaOaaan nuo IIu ana .so xv I . uhflm W xo \3 oao onnn na nInon aaon “Ina mumanIooaa n.nov~a, u oIon .qu 3 saan .aun “aoo “aouaa u > saan .aov 0 so vaI I, oan nnvm xo \3 non o nonnIono mnn xan «.no¢~n xan ouoa .Ina oaoanIooca n.ua onnnaa \3 OIoa aov u .so vaI I Ina» so n.~o¢~a nInon aaon so xv nanoanan \3 OIoa no no oan u > aov u xv .uo I I ownn v gms. .oon n.~ov~n v sun can soanIono xan :mn. “voa n nan on one: aov n xan .nn a I non .nnau ownn nInnn xan anon man sonnIono xnn \3 kuovoaoo xoa on nova: aov n .nn aInn NovmnI manna :aou xan can nvom «Hanan omnncn xaa c.no¢~n aon n “uoI quO on acanIsaan “acanIaOaaan nno I .so vaI I Inn N.ao¢~a Ina oona van on OIoa aov u .so vaI I voa so Ia\3 voa saan nao u .unon voa n3a o.oov~a oaOan xaa ao xo voa so I oaavaaonnon avanIono aov u so I .xan I v.0ovma oou na uno> naI nan .Ina ya can > \3 OIoa aov u so vaI I. voa so aa\3 voa saan nao u .unon voa n3a a. comma oaoan xaa ao Io voa so I oaavanonnon acanIono aov u so.I .xan xnvvo: vcv nan n.nn nvom \3 oao: aov n xan Ina xv ooeunL 181 _ v.vom~a OIoa aov u «a I I m.nom~n a =m.~ mmvn o sonnIono xnn nan “no I \3 an nan xau \3 nnnn oona “Ina anaa saan u so vaI vomNaI aaaovvnInon aaon oIon “qu saan “vnnon an .xan o.~om~a on vn nonnIaoaanu nomnncn nun xvnnsmvaoncn n nov a .so xv .I n.~om~a OIoa aov n no I I AaaavvnInon aaon nIon quo saan uvnnon an sxan a.~om~a on vn nonnInonnnu “oonncn awn xvnnvmvaoncn n sacs .aov a .so xv _ I up xv ownn véomua Ina oona aau nn> I aov IIu .so II» I II» c.aom~n nnnn a aoanIono xaa “Iov nan “Ina aau aov u so IIva I n.oov~a o aav AaaIvInax “acaIIna avanIono nan xan oIon «Ion Aunn>vnan “Ina anao xau nn> . aov n anaIun I aommaI I.II-,.!IIIII-i1wmeMIIIIIIInIIIIIII I , I xanII a.oov~aI anon ao xo Ina acanIono xaa uOI :mm. \3 uOI aov u .so vaI I qu II n aa Iov vnann on vn “aoo aaon saan no aoo u aov IIu so vaI oovnaI o.nov~a ava nan on oao: aov n so vaa I nOaao mIon «Iuov vmn aoIInn n.0ovua uuon “anav uoavnInon aaon \3 voa AIvzvaans aov u .so vaI I onnu Imw nanoaonn \3 OIoa on AnanoanonvnInon aaon \3 uoI aov u xv .o>aao novNaIwr vn vo: no on monncn \3 oao: aov n nn .so xv onmnnI Iva :vao scan n so xv annuaI . Ina aaa > van oonnaa . .uv aoaaa on no I van a voxaI aOI aoaa “no so aa .xan a ocasano>o \3 an Anon xxuvoonn nnu> .ava nn n "no aIn .nn .:3 vnmunI nnnn oa v.vam~a Ionu oInn aoaa . “n.¢am~n on aoava ouav ova svvva no \3 v.nnm~n 3an no I van n “a.anm~a .m.oam~a .oamnn o aunca I on n «nan Iva xaa n cm. can ovnncn “oou so an .xaa m.man~n o AaaovInax «nInon aaon anon \3 aoanInao no u aov .nao IIu .uo .a: . I m.oom~a 3aa nInon aaon onOa “aanov \3 no I oa a van aoanIaoaaan Ion «asan no nInon xaa aaon aoaaanav \3 Anonnu voaonano svvaIvvoa aov .nao IIu .HI vaI oammaI aoanInao an m.nom~a “aaoov \3 no I Ion no u Ioo nInon aaon \3 voa n uao IIu .a3 .so xv I a.oom~a OIoa Iao u an I I no .xan . o.oom~a nos “IonnIaonnam have nan no \3 In on nvaoncn nno aIn .so van I ooa na Ioo saan nao vovnaa \3 aOI nonn xan mroomma voanaooona uvnnon oa vn aoanIaoaaan “aoaaa “aOI saan .nao I .so vaI I o.mom~a 3aa Inax onOI \3 ann I voaooun “~.mom~a a oan nova xo \3 Iva gm. Ivan cnn .nn «.vomma Iono xaa “aaovoaoan 3Oa Inax o annoa a oaoa Ina nao u .so vaI I nInon aaon oIon “no aoaaan an a.wom~a I anon «an saan “soona oa oa Ivaoaaa “aOI saan .nao I aa .so xv . I 183 aoaaa n oonuaa van so xv .23 umaxooou soIcna \3 3 ommnnI “oao: soIcnn =m.n+ aov .nno oII .soIcnn ammunI onnu aannan oa vIn nannao aoa an vn «0 II Ion onan no van a.n~m~a zap oonu onOI nannao n.n~m~a aoaa .aoaaa oonnaa \3 OIoa Inn "aoanIaoaaan aov .uao oII xan .so xv I n.o~mma anon on o no aoanIono xan :ms. “OIoa aov .u so I I «.ommna onna na nInon aaon “xvn aoavvoa aOI aov u xan .so I I non «aoa no u so I voaoaanau vn xaoavvoa saan u wwlvaI omeaI n.n~m~a Ina anam saan a so xv I .o.m~m~a Ina aaa > «nInon aaon “aoanIono saan u so I .xan . I «a «.mwmma voa oa .aOI saan u .so vaI I m.v~m~a .v.v~m~a .n.v~m~a s .Io .xan w aaavInax «Ina aoanINao no I “Ina anao aov .nao IIu .so vaI mNmNaI no anov vmm unom “xomnnvvoc 2 “nos aov n an .so : n~m~nI v.-m~a n.-m~a a now “aoa no u so I voaoaanau vn .aoavvoa saan a so vaI I voaonQIoo voa I u:m~.~ .o.o~m~a @ cm. Ina aOI “Ina anao saan u so xv «NmnaI non um.oam~a o Iva nos vo: “o.oxm~n .s.oam~n .m.onm~n naIso a aanvInax “Ina aoanInao oIon “Ina oona nao .aov u vaI .a3 vIanNa non non «voaonnIoo voa aov a an IIaa aoo unInon aaon «a3 oa nao voa an saan “Asa onnvmma .no u aov aoaaa “tan xo .aoa w Ina aoanIono xaa saan .aov IIu a3 .so wv I a.mvm~a noa w xo onnn w Ina aoanIono xan \3 OIoa aov u xaa I m.nvaa @ .aaovInax «non “Iuov von anon “Ina anam aov u so xv mvaaI Inax .Ina n oaOan nnooon \3 .Ina aaa onmNaI «nInon aaon \3 voa n no: .3 an ..m~.v+ ES :5 ..m.n+ aov n no .so a o3"? . n.9nmna nan naI so aa van nonnu nanoanan \3 OIoa aov a xan .so xv I o.onm~a nan naI “Ina anao aau aov u xan .so I I . n.nnm~a nInon aaon aOI no nvoo anon \3 OIoa Ian aov a xan .so I I x3 .so voa n > aov n Ian vaI nnmNaI s.mnm~a ownn o nInon aaon “OIoa aov a soIao vaI I n.vnm~a non naI “OIoa oa Ina aov n so vaI I anvv v3 nnom 250:3 Bo... aov n so vaa :27 non a.nnm~a “a.~nm~a oan aOI onOI Ion Ina “ooa o Ina ann ao saan n xan .so xv I 185 onnn a xaa na no u nan .Ina aau oa OIoa ao xv =m+ “auanIsaan van nao non n nouan on oaoa .o saan ao xv v.mmw~n xv gn+ «no a anon \3 ann nn no n aan non =m.~+ .Hov .nno aIn .so xv .na I ownn v manna aaon aoanIono xaa nan «.oa on nvvoa aov In xaa .so xv mmmwnI .oa > on nvaonaa nvn .auanIaoaanm van aoo eon n>nn on menu nao .aov aIn xaa .so xv mmnnI m.nmm~n asan \3 >nn nn oInn aov u xan .so xv I . «mmmn o oaoa :m.e an.nmm~n n aaomoav “n.~mm~n o =m.~ .v.nmm~n o gv ana “ummnn a van ana woman 3an yuan xo .v.-m~n v.~mm~a n .n.nmm~n a .nmmnn n gm. ana aonnIono xnn aov n xaa .so xv . I a3 oaoa “avanIaoaaam nao aIn .xaaa .xan ammnaI ndvmmua nmn aonnIono “nan “ana ownn aov n xan .so xv I I «.ommma onnu an saan «voa «aOI saan .aov u an vaI I s.oqm~n nInon aaon “voaonano voa aov u an vaI I onnn an saan “voa “no: aov n na vaa onmuaI oan xv \3 aoanIono xna gmn. anmna . “asan «nonnu onnm no Ina aaa \3 voaonoIoo voa aov u «a IIaa ~.nvm~a Ioo onOI nonnm v.svm~a 3an saan a3 .xan a.nvm~a uan saan a3 oa nao “onnm “aoo “anna oaaQOaanB .oano I .so xv I I xan n.~om~a anon Ina so aa van xaa.oona aaa \3 OIoa aov u .so vaI I Ina aoan xan a.~nm~a Iono xaa 2mm. >an anon onna @ anon xo \3 OIoa aov a .so vaI I . . soIna v.amm~n Annnv «on aunnIono xaa nuoa “Ina ownn can > aov n vana .xaa I II n.xvmua onnn a Ina ann “Ina anan saan u so xv I Inov vnn anon “onnn @ Ina aaa > “nInon III aaon anon “voa vaaonn an no I \3 .Ivvoa .aOI aov IIu so xv onmuaI nan Inn aouaa aonnInuo “xowna .sxna. aov .saan so a v.omm~a unov .ana nn no n naonnIsaan naonnIaonnnm .nno aIn Ina_.nn an . I o.nmm~a Iuov von anon “Ina oona «voa aov IIu xan .so I I n.0mmfla «on aoanIono “soonVIna aaa > aov u so I .xan I onnn na voa vaoonn aa an vn aoanIaoaaan n.nmm~a no I unInon aaon aOI “Iuov von anon “voa “aOI aov .nao IIu so I I o.omm~a n.smm~n n manmm aaom xna \3 oaoa saan n xnn .so xv I ann anao saan n so xv ammunI m.wmm~a non oIon AnanvaOanIono "Ina aaa oa OIoa aov a xan I Iao IIuov von anon “aoa an . an aa .xaa \3 ana on oaoa xan «Anon saaoaonoan moovna nos aov n .so xv vmmnnI soIann xv ,v.nsm~a OIoa oa Ina aov u .so vaI I onnn a a0 \3 aoanIono xaa xan m.nom~a. cm. «non “Anannao Ina aoaovaan “no u an aoaaa aao .aov a .squn xv I m.msm~a a no “nInon aaon aoanIono xao xan o.~om~a_ van .aoo .onnu onnm n \3 aoaaa uan aOanIsaan aov .saan IIu .so vaI I, Ina aaa > am~.~+ x>nn sm+ nn oInn sm+ «oao n3a a.~om~a oona so xv OIoa ca+ “.aaIVInax .Ina anao :m+ aov u xaa .so,xv I I ana anaa saan n Iao xv nsmmnI soIana xv m.nvm~a, n.osm~n a non unoa “ana anaa xan nn> aov n na .so an I no . _ nan .nna non =m.n on a: no na no n \a .so a .xan s.oom~nw nnnn n aonan xgnvana xan ownn “vn .aonnIaonanm aov .nno aIn .so xv I an .so I .xan ~.nnmma «mnIon ana aonnIono xan “ann anna xan nn> aov n I.so xv I_ aooaaon nInon so a.mvm~a aaon xan \3 oonn .cms. n on an.ana xan nn> ownn aov n Iann vaa . I, nn .xan m.nnm~n non no noonu aoaI .>nn nn Ina vno oa OIoa aov a .so vaI I_ saan \3 an no Ina II aan ownn van voa “onnn an nno saan non v ann nn .xan v.nom~n an nnov “nan an a > «Ina anaa vno xan oa so I aov u .so vaI In anI no \3 ooa o oao oona “nan an IIaa an nanoannm “xenov van anon nan \3Vso a oao: aov n .so IIaa nonmnI EHGU anon auom .AXanymEcQU C—(c aoanIaoo van .waan .aOaaan .Ina aaa .no I xm.n+ “voa saan nao \3 oaoa an no a.:mo.+ “aoanInao _ no a oaaaononnnn xnavvuanmm aaon xaa =m~.n+ nao .saan na o.cnm~n nxcmu. vn.voa saan nao \3 oaoa na no n =n+ .aov aIn aIna .xna I saan sanv aan xaI voI an no a oIon nao .saan an.wo “anno “anon nInon aaon «an saan “aoo “aoaaa .aov IIu xv .xaa vnmnaI Inna o :m.a onnn anm> n \3 ann an.~nm~n w :a aoaaa «an no aa anon no I oIon “OIoa nao .aov IIu an I. nnm~aI n.nnm~n v manna aaon nao .saan na .xaa a.~nm~n oaoan Io «anon nInon aaon “an saan «aoo “aoaaa .aov I .so xv I Ina . aoanIono xan aaa “m.onm~n o =ms.n voa “n.oom~n xaa .so xv a.aom~n o ans.a Ioo nInon aaon “Ina xaa nn> aan aov a .HI vaI I n.osm~n u wanna aaon n.xan savann anna nan aov n IInanIun onmnnI aoanIsaan naoaan .aoo .aan na .unmnau vnvana aoao n>na m.osm~n anon: onnn na v.oaoo onOI onaa anon .aoaaa IIu saan .aov IIu xaa I nInon aaon xaa o.nom~a a0anIono xan van aaoo “aoaaa “an aoanIsaan saan .aov IIu .so vaI I an n.bomNa OIoa oa Ina nn> anaa aau aov u .so vaI . I an Inn anaa aan aov n .so a .xaa vsmunI «.momna aoaaa aoanInao xao aoaa svvoI “Ina anao aau aov u uA.IIaa I , soIanava o.¢sm~x Iuov van anon .xxaovnInon aaon \3 voa aov u .so vaI I xan ana onnn xau aov n .soIana xv nommnI onnn w :m.a xan w.mom~a nInon aaon \i Ina aaa aoanIono “Ina aau oa OIoa aov u .soIann xv . I onno @ onnu “Ina anan saan u. so xv momwaI onnn a Ina aaa > “nan .aOI u>nn Iona anI \3 o.nom~a an oonn Ina aau oa oaoa an “aoa a no I xaa am. aov u an IIaa I i m.nom~m4_ Ina no a an aaa oonuaa \3 .vn aoanIaoaaan Nao I an I .anmvnn ana aoao \3 vn n.nom~n n aoaan aaa oo n .nanon aaon \3 oaoa an amnnn aov aIn xaa I a.nom~a oonuaa Ina oonn aaa \3 OIoa aov u xaa .so xv I I n.~om~a nannoIanaoo anvaa cannon anau oano u so xv .uh I wanna aaom xan \3 nos xaInvvoa aov n so xv .xan «ommnI I n.oom~a «on aoanIono xaa ann aov n so xv .xaa I an ana anno aan nan aov n .so vaa oommnI snmma 3an ace nu aooI «n.nnm~a oan nInon aaon “non “Ina oona aOI aov u squn vaI nnmNaI . n.mnm~a w :m.~ nInon aaon “m.mnm~n o sm.~ nan .aoa “mnm~a o gm nonan «xan v.vnm~a nn> aoanInao van an no u o.aan Ina “aoanIaOaaan aov .nao IIu an .so aa I aoa nxaInvaoaaa “voa n aov n na.IIaa nonnaI xan npcvvua ana anaa aau aov nIn .na aIna I unna n saw. «an aonnIono xaa “voa . n.vcn~a no Ina oaaaaaaao nInon aaon \3 voaonnIoo voa oano a xaa .so I I n.nov~n .aaIn .aaaInvanax “nan naa Inna anaa xan nn> aov n so xv .xan I Ina aaa oona aov a IIMo xv aonmaI aoo n~.ooo~a oan nannao n.oa saaaoaam van manna m.oomna aaon «an an saan I: van voI u \3 aoaaa aoa vn oano a so xv I nonan «xnn Iao onnn w nInon aaon «aoanIsaan “aoo anon “Ina aaa Ian I .xaa > oaaaanaaoo nannao von aaon “voa soIHn oa “aOI Oano IIu .so xv oonmaI HOE “ECU MEMGm CHOm “voaaoano nanoa aa\3 Ina a \3 nannao xvn >vaoa oano a xan .so xv oomuaI s.nom~n aonnIono nov n xaa I o.aomma ann nan on oaoa aov n so xv . I xana aaavvn vaaoa xan o aoaaa oao ownn \3 ann xv onan vno oaoa o xv aov n .soIann xv nommnI xaa n.som~n nInon aaon aoaaa aOI a aov a .soIann xv I xaa o.von~a nInon aaon anon van voa oa aov u .soIann xv I IIIIIIIIIII nInon aaon “an saan a3 n.nanna n on aOanIsaan uxaI no I \3 aoaaa nao Inov anon .oano IIa .so Iva I aoaaa “so aonaon an nan “ana aonnIono xan nan > “Anaa. n.nnn~a Inax «vaaoa Ina oaoan ownn saan «Ina anao aau saan .aov a ana aaInn I anI n03Oa Iona noanan aoaaa aoaa :m.a Ina o.aanna aaa aoaa .oava xna gm. avan gm noa .aonnInonnnm saan .nno aIn xan I «.aanma nnonn aa aOI anazoIon .Ina anao aaa > aov n xan .so I I o.aanwa Ina anaa scan a so xv I Ina aaa Mcm.n “.aInvvoa aoa xn+ “Ina nan =n+ “aunan .naa na .xan . 1 .aoa =ms.n “Ina nan =n+ “Hanan .nna .voa sm+ aov n .so xv onennI «.aooma voa aan oa OIoa aov u an IIaa .I II n.sov~a «on aoanIono «Ioo non \3 Ina aOI aaa > aov u xaa .so I I xaI na n.mom~a Imomma o nn oInn oannoIanaoo anvaa oannoo anau Uano a anIso I sonNaI n.nonma non “nan aoanIono “Ina aaa > oano a so I .xan I :mm. onna .n.non~a @ a0anIono xan «nao aOanIsaan “nInon aaon «aOI oano u so Iva I a.non~a 22 as n E . I no van aa .xan n.aun~a nInon aaon xaa \3 onnn 0 :ms.a “Ina aaa > “OIoa aov u .so xv I soInn aa .xaa a.a~n~a Inov aaon «nanon aaon xaa aa\3 Ina aaa > “aoa aov u .so xv I soIna o.anmnn n :m.n .anvanax “non ana aa .xaa o.amvnn aoanIono xan aaa > “nan oonu “Ina anao xaa nn> aov a .so xv I saan xaa o.aavun van n.ono~n o .n .aavanax on ana anaa .aov .nao aIn .ana an onnmnI Ina anaa saan u so xv oanmaI o.aaoma OIoa aov u so I I an .xan «.wavma onnn w an. Ina aaa “nInon aaon \3 aOI voa oaIu aov u .so xv I onnn a IUan Iono xan :a “Ina anam xaa nn> «aoaaa “no I van nOaao an: no onnn \3 an nunn ownn xan gm. \3 ao xv gm .aov n aonn .xaa oaonnI aoan an IIaa a.oan~a Isaan “Ann> oonuvaoaaa “Ina “vn .aoanIaOaaan aov .nao I .so vaI I :3 a.nan~a an saan “aaoa. aoaaa saan .aov u .sonnIann I aoanIsaan «n.man~a w :mm.a nInon aaon \3 voa na n no: “~.mno~n oan nan “ana anno xan nn> oano n so xv .xaa onvmaI nnn o.vav~a I. . an a x, I n a a n a E . III/IIIIIII 193 v.vnv~n xxan nn>vana nan on oaoa aov n xaa .so xv a.n~n~a so xv sn noun oanna na saan .aov n so xv .n: I xaa o.annwa ana can aov n .naIao.xv I anaa Ina aau «aoaaa oonuaa .voa vaoonn m.s~n~a onaa nInon aaon \3 aOaaan no I van voa an n > nao .aov IIn an .xan I nnonn aoanInao an I .xaa n.n~n~a oIon «nan “nInon aaon xan aaa aon \3 Ina oona aov IIn .so xv I nan «.vunma .030: on ana aan “¢.m~o~n on xaIn .vnvvoa nan aov n an a I a.n~n~a aOanInao xaa “aoaaa u unInon aaon “Ina oona aaa saan .nao IIu an .xaa, I an» ann ownn na voa gm. an onna «aOanIaoaaan «an nn aoanIsaan “aoaaa a saan .nao oII .so vaI munmaI xo van onna @ nInon aaon nav :mo. u~.v~v~a .vmvwa .o.n~w~a xo “n.n~v~n n xaavvanax sms. .nan I “wanna aaon uav xaa sm~.n+ “amnsnmn an xxnav na m.n~n~n nInon aaon \3 Ina oona xm.n+ “Ina anaa xaa nn> aov u .so vaI I V n.-n~a nonan an ax saan vnvnaa “nos saan .aov n up a. I «.umnna oIoa aov a I <1 II 3&5: N ES 8.: ? E NE. é 194 anI aoaaan \3 an aonnu novnon oIon Ina OIoa so «.vvnna no a o n \3 o.aan aoaaa n .vn.ana aonnInonnnm aov .nno aIn xv .na 3 I oan .ana aonnIono xaa I gnu. oan nova owns n no ann xaa aan ~ \3 oaoa saan .nno aIn xan .so xv noomnI I aoan Isaan aono n.xv no aovIonn “nao saan .navvoa no .xan v.~eo~a nnaIaan \3 nonn an «Ioo asan \3 onnu Ina oona saan .aov u .so xv I Anooanax nao n xaa .nn unvuaI nanoa aoa an .xan o.annma xoaIIv aoaaa “an nn aoanIsaan “vn aoanIaoaaan saan .nao IIu .so xv . I «.avoma Ina anaa saan u so xv I o.avvma w an. w.ovv~a .v.ovn~a a :a Ina aaa \3 voaonoIoo voa u aau aov u squn I I noo n s.onv~ma voanvaaonaoo «0 annao oa \3 aoaaa uaoanIaoaaan aov .nao IIu xaa .so xv I m.onmNa nInon aaon \3 >nn nn oInn saan .aov a xan .so xv I . «.onowa onnn an nao saan «AI .vn .aoavaoaaa saan .aov u xan .so xv I I oonuaa onnu auIsaan “vaaon w nInon aaon \3 Ina aaa nn> oona “oao 3ao ans“ aoaaa aov a xan .so xv anomaI «.onoma Ioo Ina aOI oIon “Ina anam saan u so xv I w .xan mannna . Is I E ,2 as x s 32 E. a g $ . I; / a.mmv~a_ ana xaa > nan > on oao: aov xaa xaa «.vmona nan voanaaon \3 aOI aov .so Iva I oaoa aov xnoIso xv .vmomnI ann .xan v.nmv~a nan voanaaon \3 aOI aov .so vaI I .navanax “Inn can aonnIono xno . ano .xno m.nmv~a “oanaa oaavvon oaOan Ioo non “Ina oona xaa nn> nao .aov .so vaI I xan «om “m.~mo~n on ana m.~mo~a nnno aan n~.nmn~n on nmvmn aonn ann ownn nan aov xna .so xv I nOaao aOI “aoaaa “nan “Ina aOI aau oa OIoa .aov soIao xv .amnNaI nOaao M nouan “82 non nan on oaoa .aov soIao a nnvmaI .aoanInno .xaa .no avaoaan on ann , n aoaa «voa aao n 3 oonnaa ana nan xaa gm~.n v.snv~a away “Inn aonnIono xno .noa .nan an» > :ms. oou aov so xv .xao I , ownn w nInon aaon \3 so I “ovvma w acaaoonav oao =ms. nqnvnma .v.mvo~n o .n .aanvoaoan 3oa annx “oao: on ana aov so vaa I o.mnv~n aOI «nInon aaon \3 soonavvoa aov xan .so xv I «.mnvna Ina anao aov ann .so xv I flI I aw .so m.nno~n Iaov von aaon unInon aaon .aOI .voa aov u so vaI onnNaI xan o.aovNa "683 23 non ES .83 aau aov n .so vaa I voa n aov n ao o>aao .m.n+ oan anaa nuanaoav onoa sanaonam voa n nov n soIao vaa 8.3+ aoan nOaao I Incaao “voa aOI aaa oa onna nanoanan \3 oIoa .aov a soIao vaI coN+ Io .xan o.vwoNa non naI «Ina aaa anan oonnaa \3 OIoa xao aov a .so vaI . I I Ina u aOI onOI aoaa xnvaa o no .non naI .xaavInax .Ina Iuv aaa “non .nInon % aaon \3 aOI .voa ans.N aoaa “Ina oaoa :ms. van 1 Ina no: :2.» «saan vovnaa \3 onmnao x3 oonnaa so xv «.262 “vaooa Ina w asan N .anan Ion Ina oona aaa > an aov .ana vaaa I nInon aaon I xaIanoa 3 “non aoa n sm~.~ "aonnInonao ran nonao ano .so o.avvna non Ina aaa anaa aoaa “aoanInao naoI “non :mN.N .aov .nao u xv .xaa I aoanInao “saan vovnan \3 nonaa :73 ann .No onovomn xan oonnaa nan ana onna non noon o gm ana x3 3o :3 En xv .x3 I I soIao mémvna onnu nanoanon \3 OIoa aov u Ian vaI I soIao nInon aaon oa voaonoIoo voa aau aov a Ian vaI omoNaI anI oaasanovaa no none @ nnaIn . o>n 0 man 1: .353 a: 1: Q .1; . 197 voawwna aoanInOaao OIoa nOaao a soIao I onnn no na saanaooonn aoanIaoaaan a \3 anIao \3 aoa aov .nao u Iao .so I annNaI I an n.onnNa a voa «Ina oona > .aOI aov a .so vaI I onnu Ina u \3 aOI voa a aov u unIso xv onnNaI aau onno>on N.oonNa Iona \3 o.asvun oan noa voa n “noa “ana onnn saan n xaa .so xv . I so I .xan n.hsoNa Ina anaa aaa saan u .so xv I ao n.osv~n aau aanov \3 xIvvoa van aOI onOI sao>annonoono aov u xv .so xv I ~.nso~n oao annon no n nan aoan “manna oao o.aan ann aonnInno no a on n so on van ao nonao ao v.osn~n aoaa “o.aan Ina anao aaa no a ao oaaaaoo aaoon .nao .aov IIu xv .so xv . I , o.NowNa Ina anam saan u so xv I no nao .saan xan aao oa vvo van nInon aaon \3 aoa “xIvvoa saan .aov u .so vaI aonNaI xan n.oowNa xom aonnIono xno “ana anao aov n .so vaa I anov vow anon “Ana nvvoa .aoa aov n so vaa osvmnI xan m.onnNa u . Ina qaaq gnu xoa Ins E noaao uaoaaa “oan o.aocfla nInon aaon \3 onnu “voa a aOI oa voa I oa u aov xan .so I . aaxz mvoa n \3 gm. annao nao ownn “.onna ooaovoxooan xao n \3 o a .oaoa nao .nov xaa .so a onvmnI saan nao o.anoNa \3 an onnu “vaaonn anI xan aoanIono \3 voa oa saan .aov xan .so I I v.nnnNa onnn o Ina xaa :mN. aaa «Ina anao aau oa oIoa aov so xv I. . :a annna aa nnaaIna , van aoaaanav onoI oaanooa voaonoIoo voa a aan aov so I nnnNaI aoaaa xaa m.onoNa “onna w aOI “Anav aoavnInon aaon \3 voa a > aov .so vaI I ‘ o.mno~n Anav aoavnInon aaon aau “Ina aaa aov so xv I Hanan “non “nos nan n aov smevIa manna..— o.vooNa nan “Ina aaa aov an I .so I I a0anInoaao sanv Ina oona onOI onan “n.nnnNa an I .so n.vnnNa oan nao ana aonnIaonnam o.aan ana anao can aov .nno xv .ao xv I van \3 o.aan noaao no «.noona nao aonaa “aonnInoaao “nao no on \3 ana can .nov an .ao xv I nOaao ao a.nnvNa aoanIaov van noaao “Ina oona aan .aov vaao an I no I ofinIaoaaam axonoo ans» novnsvonManzmm MWMmmvma on x; Ema 2:“ > E .E $5. 9 9 1 oooNa San Ina > Iona m.oovNa xan a.oooNa oan xaa anaaoIon «Ina ooa aa nan naI “Ina aaa >I aov a .so vaI I b.0owNa voa u aau oa OIoa aov a xan I onnn n no Ina anan aaa :a+ “non naI m.oonNa .ana aaa ans.n+ «oano» aaon \3 Anvvoa nos =m.~+ aov n no a .so a I non naI Ina aaa :m.a annnn uvoI an , “Ina voaonoaoo oou o noaan n .vn .aonnInonnno aov .nno aIn nn a .so a oovunI o.aovNa Ina anan aau xaa nn> nao .aov IIu an .xn nao I ownn aov .saan xan v.nonNa w nInon aaon xaa “aoaaa oonuaa xvn .aoanInao .nao IIn .un aa .a: I n.wovNa Ina anaa aaa :m.a annna “Ina aaa oonnca \3 OIoa aov a so xv I Ina OIoa o I cm.+ "OIoa an :mN.N+ so I “ana voaonoaoo =~+ “vononoaoo voa no =ms.~+ aov n .soIna an vovmnI voa aao von “gm.n non n.nonNa N.monNa o nInon aaon aOI oaoa “aOI u aan oa OIoa aov n so xv I :mIN Amman aa saanaooano nnonn aan non so xv oaoa “azov aov .saan squa I noaanan vn oou na sxao xavaonaa nvn aonnIaonnnm .nao a aIna .a: novmnI soIna Ia.~ov~a o I van a o.aan Ina anaa aaa aov IIu xv .so I I o.aoONa nonan n nan on oaoa aov n so xv I aoaaa mom *5 a» H. co: ago \3 oaavanonnan o.aonNa . a E on E E 2 1s «a . IaOaaan o I uo In: as \x E a a x3 a . Sakai aoanInuo “gms.~ voa on \3 ana aov .nno aIn .so vaa I I .m.nns~a onnn @ non “Ina anao xaa nn> aan aov .nao a so vaI I xn.aonan “vn .aonnInonanm aov .nao a so vaa nns~nI aoo ana xaa o.aasna voa aau oa oaoa «oonu aon non “Ina oona xaa nn> aov u .so vaI I ,ao ana aan oona aov n .sonvIa onsnn..: QOFNH w an . aoa .oavvoa “m.nos~n o mmov naoaaao \3 an onnn saan no .xaa o.aosna ownn no aoanIaoaaao xaa on so xv van no no n .Hov .nao aIn .so xv I o.aosma o gnu. xaaavanax “Ina manom xaa s.sos~a aaon xan \3 voa u nIon .Ina anan aaa oa aaa > aov a .so vaI I voa a on n aov n so vaa sosmaI o.vos~a ana pan on oaoa aov n so xv .xaa I so . «.mosua saan .aov n ava .xan I voa saan u oonuaa “Ina anan aaa nunosua m xaaaaanaxInanaImmemwg OIoa nao oaov .onxo..xnaI. oosnnI_ aINOBNa aOI aanon anaa xan am.n aa Ina u oa voa a unInon aaon anon “aOI aov a .so vaI I ana anno saan n so xv nosmnI . so «.vosua xaa aonnInno “ownn “voa no voa \3 xna saan .nno n Ina a xaa aan omno>onoaa a.v~s~a “woo aoanIono xaa “ann anao xan nn> vno aov n xaa .so xv I Ina anao aov n so xv mnsmaI I n.NNoNa onnn w Ina oona u \3 oIoa aov u so xv . I nOaao I xaa «on ana xao n > oaom “ana anno nan .aov n .soIao a mnswnI Inov von anon uaoan noaao o.aNoNa Incaao “onnu nanoannn “nan “Ina oona aau aOI .aov .nao IIa soIao I I nOaao aoanIaoaaan onOI van aOI onoa ans >an nn oInn .aov .nao IIu soIao I aNoNaI Inov von anon aaoan nOaao n.oaoNa Incaao «onnn nanoaaan “non “Ina oona aan aOI .aov .nao IIn soIao I . I vaooa n3a na ao oaoa N.oasNa . “aoanInOaao .no u .Ina oona :N+ “aaoxooov nOaao N.oaoNa nnonon saoaoaoIoo aoa vaaon o no I aoanInao .aov .Nao IIu soIao I I n.naoNa aonnIsaan «ana anao aan nan saan n xaa .so xv I N.oaoNa oaoa aov n xna .so xv I nao .saan a.naoNa aoanIaan .aoanIaov nnOI Iona .aov a so xv I xaa .aa Ina voaonoIoo voa no “Ina n aov a I .so vaI maoNaI ao no acaanoanaoaaan oIon .Ina no I aa naaa mo aoaaa onan xan .un «.vauna xvoa ownn Ina .uo no I van a o.aan Ina oona aov .nao IIu I .so vaI _ I] 202 I xaa a.avoNa aOI nInon aaon \3 voaonoIoo voa u “aoa aov u .so vaI . I xan n.0voNa v.ons~a van m.ons~a o .aavm anax “Ina anan onoa nao .aov n .soIao I I xaa «.ovoNa vaoon on w voaonoIoo voa a «Ina aoI aov a .squa I I no a van xaa «.ovoNa a voxaa ana n aoaa .sxao moov .ana n no :m.n aov aIn .soIna a I s.ons~a o anon aaon \3 oaoa aov n so a onsNaI v. onoNa van n. onoNa m.onsNa o xaaovanax .Ina aoaaanav onOI .Ina anaa saan u xan .so xv I wanna o cm. xnaavanax “ana anao saan n so xv snsnnI N.ansNa onnn w Ina no I aaa \3 OIoa saan a so I I aau onno>onoaI “Ina aoanIOano oonuaa “Ina anaa saan u mmvxv anoNaI o.oNoNa nInon aaon \3 .oaIIv voaonoIoo voa .aoI aov u xan .so I I I s.n~s~a OIoa aov u so I I ana nan aov n so a onsnaI aoaaa xan n. oNoNa \3 onnn a Ina no I “Ina no I van a aan Ina aov Ila .so vaI aoaaa “anI xan o. oNoNa aoanIono xan uo nvoa AIIuvvoaonoIoo voa .aoI aov u .so vaI 203 xan «.ovhNa .amN..n onna na Ina aoanIono xan “Ina oona aaa nao .aov .so vaI I ao a.ooswa aoaaa “nInon aaon anon \3 voaonoIoo voa aau aOI aov .so vaI I xaa .ao s.sns~a nInon aaon nav aov .so vaI I ao o.avswn nInon aaon anon \3 voaonoIoo voa aau aOI aov .so vaI I _ I . «.snsma aonnIono xaa non “xaavanax n “ana aan aov xaa .so a A I m.mvs~n o Ina aonnIono xaa :mn. «ana anao saan so xv onsnnI Ina aOI oIon “n.vvoNa xan a.mcoNa o noaaman Isn “nan naI “Ina anao xaa nn> aau aov .so vaI I I voa I aov xan .un vvoNaI onnn w an m.nsza Ina aoanIono xan :mN. “vaaon n3a na an Ion OIoa aov .so IIaa . I aau onno>onoaI N.n¢oNa unaIInaa «moo aoanIono xaa «Ina oona aaa aov so xv .xan I soIInn a.ncha aonnIono xaa noa .ann xan aov .so vaa I o.asza non aonnIono xna .ann can nov xna .so xv I ca soIana m.ans~a Ina anana “aoanIono xan aoa “>an anaa xaa Ina aov .so vaI I n.a¢hNa «on aonnIono xno .ana can aov xaa .so xv I soIao a. o.nms~a onnn ana n .noa aov n .so a .xaa I soIao . v.nns~a aOI aov n I .so I I . a.nmoNa aaa no I .xaa no a .Ina anan xaa nn> aov IIu so vaI I aoaaa vnIaaoa anon \3 OIoa saan .nao IIu mwlvaI nmoNaI I n.NmoNa Ina anao vno aan saan u so vaI I xaa o.amoNa Ina aaa oona aov u .squn I I xan ¢.atha Ina onnu “voaonano voa .aOI aov u .soIao I .IL voa \3 oano» anon xno nav n~.oms~n xaa m.oms~n o :m.a «nan oIon “voaonano xoa .aanvvoa aov u .squn I I xan a.omoNa Ina anaa aaa > “aoanIaoaaan saan .nao a .so aa .a: I onnn oa aaov OIoa “no I onOI \3 noa na aOI aov u Isqun I omoNaI onnn w xo “n.osza g cm. .o.ons~a o gmm. .m.ons~n o gm. .oon o gm. nInon aaon aOanIono xaa “ooa na Iov nnoa Ina n.ovoNa no onna o Iov I nnan no vno Ina “AnanoVOIoa aov IIu so I .xaa I «on «a .xaa n.ons~a aoanIono xan “Ina aamov \3 oona Ion anan aaa aov u .so xv I nonao s .xaa o.n¢s~n oaon “voa oona s oa \3 .Iuov von anon .aOI aov u .so vaI ll 205 . . an s.v0hNa won: 0 nInon aaon “an sn so no aaon “aOII aov u .xaa gso I I n.vnoNa onna w aoaaa \3 nInon aaon nav «Ina anaa saan u so xv I xaI xan «nnonn aoaaa oaaannonon an.ansNa I o gn .¢.nosun o gnu.nvana aoanIono xaa “an: no so u.uouun a van n no: xanvaa onoo anan noa on gm..aonan saan .aov aIn Ina a .xaa I IIN .xao o.aouua oano o ann aonnIono xao gm.n “anI nan nov n .so an I aoaaa “onnn o asan “am.N annno aa nInon aaon «:N a.anoNaI aoa vovnaa ax .voa nao saan aOI “Ina oona aau > saan .aov IIu squa I I n.oosNa Ina aaa oona aon aau aov IIn an .so I I n.omsNa aoanIaoaaao .uuoa no gmu. .soIna a .no nvaoaan saan .nno a xaa I III na n.omsua ann ownn can nan aov n .xan .so a .I I gm.u annna aa nav xaa Ion nInon aaon \3 AIIIn .aauvvoaonoIoo voa aOI aov u .so vaI onoNaI a.mnoNa ann anno xan nn> saan n so xv .xna I .aaavInax oaoan 30a “Ina anao aaa nao .aov a INo Iva onoNaI .n.mmoNa OIoa aov u so I I ImoIao I ana anao aan aov n .so a .xaa mnsunI saan mgooowa oaoa n so va , n.onoNa1 nn nan “.aIn .nanvvoa aov n no .so a. I I . a.onoNaI nInon aaon \3 Ina aaa > aov u xaa .so I I OIoa aov u no I onoNaI aonnIono nov n .xaa m.nvsun, . n.nvsuafl ana anao aan nan aov n xaa .so a I I no .so unvsuaw nnonn voa aOI “Ina oona aaa > aov u xn .xan I_ ngoosNa a0anIsaan “OIoa saan .aov a so xv I, s.oosua_ moa na nInon aaon «Ina anaa aaa aau aov u so vaI II n.nnoNa, xonIa .uanvvoa aov n so a I, I «.oooNaI Ina aoanIono xao onna w :m. “OIoa aov IIa xan .so I . I vaaoo 1 a Iuov von aaon “an. annnn aoaaa xnInon aaon an N.nnoNa_ anon «onnu an nao saan “no I anon \3 a “aOI saan .aov IIn aa .so I I an s van so aa “nInon aaon s .so N.mnsNaw aau ana «xaI no I «xso I .no a .am. oa novaoaaa aov .nao I aa .xan . I voaommwoo voa a aaa Ina oIon .Ina anao xaa nn> aov a No vaIx mooNaI, uInom aaon u “no: I van aov u no chI vnomaI «.aosud Ina Inan scan u so In I w.oosua oosma oan an “no: u voa “manna csom son I Isn .so go I n.oss~a and asan scan u Isn .so xn I n.sss~H o aon Aficsvmaocn 30H «a .xsn m.sss~a nan Ina Inan can» w.noo~a 0» I300 mInmm Iaom aov u .so onI I Ina :naa Io n.moo~a In» un> “oou a scauIaOaaam “Iumn cum uuom .uOI aov .nuo IIu .so I .23 I .No _ .uo : \3 In nan. pan “and squn can so 2 Hon .suo aIu Inn .so a mssufiI m.ess- ooun o and non “Au >vsoucw “nosuIHosHsm Hon .uuo a gun I In so .xsn «.ossuu Ian moo “ADIuvuOI aov u .so vaI I EnH ucmn an xnu =m~.H o.assaa nan sax: onuu use \3 Hopes :m~.~ nu \3 oao: Hon u so go . I xsn o.assaa Ina :nam In» > aov u .un .so I I o.assma CID: scan a so I I ownn s.oss~H o nosquuo as” so can an \3 Aucu “.uo: voa Hon u squa 3 I w.oos~I mans w x0 unnauIaon «DID: aov u soIHn I . «.oohna ucu mInwm Iaom mom .OIos aov u squa #0 . I an. and onuu uoa Hon .uuo u .so xnIa oosmuI nooma cu m: ocammaI nuoo “Ina ans. N “a.noo~a a go .m.~os~a a g. aoH coda an» ucu “o.~os~H o cw .~.~os~H o sn no: u .uo u “s.~os~H _ w :m.a .o.noo~a o :mo.o .Nooma w :mN.~ qu soak szcn an v.voo~au Iaoaaau no I “AI 0» u .un can so cuonvno: uOI .aon .uuo OIu .so xnII I_ no u can 0 on I o.aan «Ian .Iunn .uomiwwuu “Ina aon OIu an .mo I noonaI oao Hon .azcn aw m.oos~a onUAIIao Ina coco “aau ocaon Auo u .:a on asvaouca .uuo OII Ian I .xan I m. , 33 m 62.3 _ I00 no I can u o.aan .Ina onus omua xnu In> aov IIu .so xnII I «.ooswa 3H: and owns “manna o.aosna Iaou “Au 0» I .ucu aouvnmuonnIoo no: “uOI aov u so xUII I n.5oona Ina :naa In» un> ucu aov u so xnII . I omua .zmm. cIn gm. no v.0oowa .~.an no a Ian “xua go a o» u \3 .ucu .svno: Hon eIu xnIa .an I_ and undo as» ucu Hon u swlxn oosNHI - «.mosuaw uoa ucu Hon u so xn I“ o.vmo~a_ anI asan ucu scam u xInIso In I" 209 onuu w.¢oo~w xan as» can voa saan :mu. Iao oouuaa \3 OIoa saan .aon u so I I can .xan. m.qoo~a gm. m and nosquuo xan “an” scan as» Hon u .so «I I «.voona Ina anao saan u so xv I Awo I can I xaavo.~oo~a o gas. Ina an» “oou u: sou gm. ana n.noo~H_ an yo I “gm. 0» a: oouuca Hops“ “noauIaoaaam Hon .Nuo aIu In .so a .I «.Hoouno and can > son I can .xan IV n.Hoo~H aouaa .oao: uoa Hon u an a I a.aoo~a auuca a nan voa Ion Ina Hon u In .so ya . I _ m.ooo~am oao: aon u Ian I «.ooomav oao: aon u an a I. nooaa w sm.~ .~.oos~a o cm voa “o.nos~a o =ms.~ so nan w.oos~H g cm “n.mos~u o ga .H.nosma o =m~.a Iao xn .so «.oooma acauIIOaao Io .nuo .aon ownn Ina .Ina anan aau aov u I .un I. II moIao xn a.oos~a no: uos Hon u .un .so a“ I. :oaquoano “oao: Ion u soIao xn oosdee . us o.aaoua .aeusa usu \3 usaeusa son I .so anI: . I sesquao so .eanem ssse us .sas s.ooo- saoe .nos suaeusssn .ana use uoa .aeusa .uoa .use .aon u .so snIa I eso “sesuIssse n.osans nso sequaoo > oou us Ina sas ssu “susu Hoo son a xas .so so I” see son a as anI: oaoNHI ~.ooo~I_ nuns o oao aoau aoo anon mom “Ina anam as» > aov u an xnII I_ uano aa .uo I .IOaIquo :a+ “aoau uao .saan I Iuse sous .uo u .uo: «.sssvsequuuo .seusu .uoa .uuo aIu us a .sss oeouaIw n.ooo~H_ mInwm aaom “IOI aov u IoIs I no: oaaoaaouuan nInom aaom uann \3 no: u > aon u Mqun xnII nowuaI oéoofiU sesuIsssu .neauaesaae oases uaaouum sssn .use I us I_ III «.sosms W ans oaes son u as I avaIIsaan «mInmw aaow xan onun _ ssu “see neuuseaaau “neuaue ss Hoes oases one use .Hoo u so .us so scamsI, m.moo~a, no I avauIaOaaam “Auo mvzmo. ou I: aouaa saan .uHo I so I .xan If ownn on Ina HOI voa u “Aao I no . ueseoo euosvs.moons o maeem saom ou neueeoaoe . . so a .so m.moo~a .eos oa “oou o :m.~ sea uss .seaquuo gas son eIu Ian I .sas I_ 211 o.ammNa aoaaa .aoanIsaan saan u so I n.n~o~a non an no 0 0a I \3 OIoa Nao .aon a un IIII I Aa0aan0auaoaaamvomnn . o.d~o~a o Ina aoao no aoaaao I anon \3 Ina an aOI aov .uao IIu an aa I aov .waan m.-m~a son sns ssu n “osnsse sennInennnm n .uuo aIn so anI: I o.aaoma I «.muoma a .anVInax «noa na Ina no I aaa anom “Ina anaQ saan IIu so vaI I «.oacua aOI n aon u so IIaa I aOI u aon u no onI mammaI n.5amma Ina aaa oona nao .saan OIn so vaI I n.5aoma Ina anan aau oa OIoa scan a so IIaa I no u :a 0a 99 a0 “ownn .o =m.n neusn “no a \a no nos ss oenu ownn sen o.mno~n no u .Aonao no sn o.aanvIna anaa “aoanIaoaaam saan .nao IIu so I .23 I m.vam~a o :n .qnoun a =m.~ sen sens ssu usn ue.~no~n o sm.n so a 050s “n.¢no~n o =m.~ .n.nno~n o :m.o .o.~am~a o :a .maoma o so voa so an n aOI aov u so vaI manmaI oaos ou uoa nee n so snIa mnemnI an m.aao~a aaam Iona aoo “aaam oIom .aoaaa aao .aoc u .so chI I 212 J eons .so us .ns o.anonn o so no: «on sesnIono sas “eon sons ssu no> nao n so .sns I no ua .ns n.~no~n uoa eons o gm. sans sons ssu no> son I so..sas I «.nnonn o so “oneno mIsn gm. oos squa “ans sns .NwIMMIqN on ones oso so. oos ssso nae “ans sons ssu no> Hoo n .us soIa «nowsI =ms.n . IINo scans on sns sennIono “nos “smsnem snow msovaon nao u squa .sns nnounI .s.ono~n oaos Hoo n as soIa I ssso ss noes sns so .so n.ono~n “eons o ans sun so noes on > n > so so \3 uoa aoo u so .ns a I o.o~o~n sun uesnuouosn ssu \3 sennIsennnm noo .uuo aIn so soIa I m.o~o~n mnonn a0anIaoaaam \3 Ina u > aOI aon .nao u so IVII I so so ownn na Ina aOI “nan “Ina oona a > aov u .so IIaa. ommmaI no.o~o~n Ina onnu aaa > “aoaaa “aOI aov I so IIaa I o.o~o~n Ina aOI u oIom “Ina anan aaa aau aov u so IIaa I so squs no sseu amen sonoson ou n oos ssso .soo u a .sIus a ouonnI Ina anao saan u no so ..o~n~aI an aa «.onoun o oos so so u uoa =m.~ “son sons ssu aeo u .so soI- ono~nI snsvanss us sues “no a sennquo \3 no nos “ans sons ssu noo u .so aIus ononnI” m.sno~n_ suanInao .oonn na voa ma oona u \3 OIoa saan .nao I. san .so so I soIns n.sno~nu sennInonse .aun ssu =~+ noses gn+ Hoo n us .so us I_ I ssso sas .so s.ono~n scan at aa Asaan aoovcao: sanvxaI cam aa aon .aoo .Nao u so .a3 .HI I I «.onoNno sonueeo son on oos one us s “on .sennIsennnm soo .uuo aIn us .so a I. as oénoun ._ ans ssu noo u us .so us I ns ménonn I aoanInOaao “Ina anan aov u aa .Io xv I_ a.wno~n_ aoanINao "OIoa saan .nao UII Ian I OIoa soIInn , =m~.n sesu “ans uses n =m~.n sesu sues =m~.n noo n so .so us «nonnI m.nno~s, oan .sann usuvoaos aoo n sas I ~.nno~n son ssu Hoo u so a .sss I o.anomnw OIoa aov u so I I Han «ownn w mfimwm n.0mwfla aaon Inn so “anI «noaonQIoo voa I aau oa OIoa aoc u soIHn aa I. DID: ao I no a so. no.ooo~n o oos so so on \3 so .o.ovn~n o :ms. .e.ovo~s o :m.s .sou o sms. senn Iono sss :uneieonn n \3 nouns 28s so so on nao n so so .sns anon? n.oon~n Ina anan saan u so so I eons o sas emu. oso son oos n > sesu “son osono ssu ssum \3 s.o¢o~n OIoa an no u aoaa sooa o no I “Ina aau oa OIoa nao .aon IIu so aa .nn I o.soo~n Ina anao saan u _.so so I I ns n.svo~n sns no noneusn n usennInennnm nuo sIn .sns .s: I ~.~oo~n o :ms. son so s “son sons ssss n INo soIs scounI I ns n.~eo~n .gn ou so ne us no noseusn “sennInennnm nuo s .sns .so I m.non~s Inna anon Ina no u aaa aOI \3 on .aoanIaOaaan nao IIu so snII I noaonano no: oa 0a a .aOI saan u Jmo scII avnNaI ns ua «.oenmn son ownn ssu noo n .so soIs I ns ua eons o so sennInonse uos noes n sues n nao n .so soIsI oeonnI ns ua m.onn~n uos soo sIn .so soIs I n.omwNH. Ina anan saan u so xv OIoa aov u NW I. annual s.nmo~n son usn nao n sns I «.omonn osos Hoo n sas I son sons ssu > noo n .INoIns a omonnI n.sms~n son ssu “nos «sennIono nao n so us .sns I 5 son ns n In “son so .so use n \3 sn m.smo~n Mu sn :m.n n=m~.n ou so He no n .xus no s .neusn soo .nuo sIn ns us .sns I n.¢mo~n son usn ou osos “m.nmo~n o =ms.n “sssneusn no s Hoo .nuo sIn so soIs I sas ,Ioa ovno osos noo n soIns ua nnonnI so us m.~mo~n aoanInOaao “Ina so aa aaa \3 OIoa aov u .soIIo xv I ns «.nmons Iuov von anon “aOI oa OIoa aov u I .so vaI I , so: m.nmn~n suosvuse sues use .Hoo n .ns .so so I «.nonnn gm.n nouns sas osos ou oeueossoe oos on soo n sas .so so I m.ooo~n, sennInensnn “sue son sen .gmn. n sonvneusn nao .nuo sIn so a .sns ~.oon~n Ina anan aaa aov a an I .so I I o.mon~n ao vn .Ina onnu «aOI u aov u an I .so I I ns , uos n Hoo u .so sIun moonnI_ ne n “sennInennnm neue sas .ns «#32" n3a aoaannnacoa \3 no I :m.a “nan “Ina xaa nn> aov IIn .so IIaa I >sn so ua .ns n.nnn~n son sn oos n “nuns o ans osos sns an “son ssu Hoo n so .sas I. osos nao n so sIua noonan xanIMNo a.~wn~a aoaIa “Iuov von anon .xoonuaavnInon aaon “voa u nao .aov IIu xv .MI I In m.noo~sn ownn w aOI oa OIoa nao .aov IIu so.I I so s.non~n. onus o so so \3 son ssu aoo n so .so us I eons o oeuenssoe snooos uos ou osos aoo n moIns ua nonusI. s.ooo~s osos Hoo n so so I“ an no s \3 use no n ns .. . eens woos o “n.ooo~n o so “son ssu no.omo~s o nao .ssss ‘ ns o.aoonnp :mm. oso sou o .sns .nsvseusn .on .sennIsennnm .nuo sIn .so .sas I” 217 m.mtha Ina aaa «vn .IOanInao aov .nao I so I a.msn~a 3an I n.moona no I anon “Asxanvonnu voaanano nn> n \3 OIoa aov IIu so I I w.vso~a an ..o.voo~a o son ssns oenn ns o n nos. “on “son «sennInuo neo .nuo sIn .so soIs I m.oon~a vn “Ina “IOanInao aov .nao I so I I .sna non senn uosvm.nso~n o gs neusn “sns oenn enos oso nos no.~so~n ass no sns .ns n oso no a “sun so a ssu \3 o.uno sns ssu son nao sIn s .so a osonnI o.aboaa o.nso~n o son sennIono ssu sns so.I “son sons ssso n so so I use eons o son ns smsso o.anonn ssu us noenn ssu sns so ou sns \3 oeueessoe oos use .Hoo n .sns .so a I m.oso~a voaonoIoo voa I aau aov u so I I N.Ohoua OIoa aov u so I I nan naI “Ina anaa xaa nn> aov II“ no I .. nonmaI m.onn~a neaao non .ao an “Ina aaa > aov n so xv .xan I :mIM onnn aOI “onnu au onnu no I unnosna no I aoan so a.onn~a Inensne \3 o.uno son us no n gm ou =m.n ownn nuo .noo sIn s .soIns s I ssso , s.soo~n nao voa saan usuanIaoaaan “aoaaa .aov .nao oII soIHn I I sns .so osson amp. saanneesne .oos sennIsssn m.¢nn~n so “seesues sn sns ssu \3 ns cos. .aun ues neo n Ins sIus I .. «nonnunh uos ssu .usn ou osos noo n so soIs I onnn na aOI oncI .nan .Ina anan aaa :m.o+ xan sNoA .n.nnn~am “sneo oes unen .nssee ues sns \3 ns uos =m.~+ noo n Ins soIs I eons oso sou o oes oenn ns s \3 son usn ssso n us .so a nonunI_ n.~oo~n Ina aaa > saIn u xan .so I I OIoa van Iuov von anon o.aan m m.ann~aI nonnn @ van vaaonn no I \3 an voa .4:v+ “no I \3 an onnu aau OIoa .ooa w nInon aaon ns :m.o+ “eons a sun so. sns \3 son ns =m.n+ m.noo~n “nee .oos use on n > .so \3 mseem saee :~+ use .neo sIn sns .ns s I o.asown. sax: gm~.n neusn sen noes usn ou osos nao n ns s I sns «Ansonn ssu» “son .usn .n.seusn non .sennInuo noo .nuo eIs .ns sIus . I son ssu .sennIsennne soo .nuo s ns sIun ssonnIe s.oso~nm oeuesssee Assoc: soo n ns sIun In son ssu so oonn .uos e.oso~nI use ns on gs \3 nus sns =~+ “son ssu so ownn .uos gm.n+ sesame snow “son sns ¢.oso~n ssu so ownn .ues sn+ «son ssu “on .sennInuo soo .nuo s .soIns so I gm. oes ssso nse o.soo~s «anI Ina aaa > no ao vn oao svn .aoanIaOaaan saan .nao I xan I nnnn a nInon aaon .so I .OIoa smo.a saau onno>onoaI .nan o.aonma .Ina onnu .aOI sn+ “non .Ina anau aaa :m.~+ aov u so vaI I gm.~ sou ss osos ou sns ssu > soo n sss soonsI vn aoanInao .anaa Iov no a “no a \3 sn nos ss eonn .ns no n gm.~ .se nuo .ssso o.aoous no n on seuss gs+ .ge+ o soon ns ssso .sos ssu .soo sIn I mou o ans sss gs “nus n sss “oes ssso so s.ooo~s goo. nse \3 «on .suosa enoe sosu nosvseuss os soo n Ins s .sss m.ooo~s nsnos oeusesno .so usooos n > \3 osos soo n sss .. I sns .sss m.ooo~s o gs ues “eons n > \3 sns ssu > ou osos nuo .soo sIn .so soIs oooosI o.aoons oona .nInon :aon aov .Nao I xan I soIns m.ooo~s seuss no n ns \3 on .sesnIsessso soo .nuo sIn I I .so xv suns: once sosu neos ns no n ssu so U 6:" ~ n: F” '01: E EEEEWE— gs .ssns onnn nooseuss os \3 on .sesnIsessso soo .nuo sIn Ins s .sss soomsI xoa aaon «.onnua sonnn Iona sa vIn moa na nInon aaon \3 OIoa aov u so I I sns so >nn anon .xan .so osooo sseo “eons o sns sns so gs \3 sns usn soo n Ins sIus moomsI s.moo~s eons o gms. sss ssu > .osos soo n sss I No o.¢oo~s sss osoeo ssoo .nss ssso .soo n usIsa .sss I o.¢oo~s sssvsoss .o.uss ssu > .ssu usn sen sss soso soo n so.I I onnn a nInon sson .no so go. .ssse gmn. on nse .xus sss nosse «.ooons \3 ao oao ocaaanaaoo onnu aaa \3 an no u OIoa .aov IIu no xv .up I nInon aaon an “was .oos ns n > .ssInsseuss usn .on .sesnIsessso soo .nuo s .so soIs voonsI n aoaIa .onnn na nInon aaon aa voa aaav .no I anon .Iov no a: m.non~a u sooa na voa saan nao am. vn .nInon aaon .aOI saan .aov IIu .xan .so I I nos .usn sss ssu s.soo~s sssso nse .uos .osoeo ssoo sons s.noons onsseuss gm.~+ “oeueoosoe oes usn ou esos g~+ ssso .soo n soIns soIs I .gm.ooos ssso o.soo~s nse .suos sss ssuose on ose .on sesnIsesssm ssso .nuo s sss I ownn w nInon Iaon so voI OIoa smo.a+ saau onno>onIoaI o.aonna .nss .ses oonn uos gn+ snss .sos ssu sass gm.~+ soo n I , nIso show. I .1 I I1 ssu usn s.soo~sI sssso nse .uos .osoeo ssom .ss s.noo~s onvseuss gm.~+ soeuenosoe oes usn ou osos g~+ soo n soIns soIs I sss s . soous. sns ssu > .uos soo n .so soIs I u saan nao .voa onnn xan o.acoma Ionu cm.a Inon aaon \3 voaonnIoo voa oa OIoa aov u .so vaI I s.ooo~s sns ssu usn soso soo n so soIs I sss see nos .soensssos ssu soo n Isns .so a ooonsI sss o.oon~s nos os s .ooos o sssIsns gs \3 osos soo n Isns .so a I n.ooo~s seuss .sos ssu uos soo n so a .sss I nan naI .aOI aoan Iouo sn.ooo~svgms.s .s.ooo~ssg~ uos .ou ns oens sss ssu sen g~s+ “sesnInuo .seuss on n > no ns s.ooo~s s sss gs+ sass no a ssu n \3 sns usn osos go+ soo .nuo sIn .sss .so a .. I IOanInao .aoaaa an v.5onma on n > .no a sss spoons eens “sns usn oses soo .nuo sIn .sss .so a I nsIso o.ooo~s nQIIIan aan saanaanno .aoanIaOaaan xaI no I aov .wao IIu IIaa .xan I van aoo3aon ma0aannnmon v.woo~a aaa an no I onnn a oaoa an no I onnu OIoa nao .aov IIu so I I 3HQ “Ham #0 aoanIono xan sa+ sonnn van Qoa w nInon aaon voa onnu OIoa so I sm~.a+ “voa u oIon \3 OIoa aoan n.mon~a Iono sss gs+ sossos o oo: ownn ones so s gm~.s+ soo n sss .so so I onnn aoanInao sonnn o osoeo ssoo uos sss "snooos.ssso soIss ssoo sssn sss o.oso~s van nao aaon «no I anon \3 no u svn IIuvaoaaa .nao .aov IIu .so vaI I n.oso~s . osos soo n so sIus I ~.ooo~s o gs mason ssom “no s \3 so ns no n ss nos «ssu usn soso sen ass “on .sesnIsessso soo .nuo sIn so sIus osonsI o.soo~s ooa na anon no I OIoa nao .aov IIu so xv I «.soons m.soo~s oso s.soo~s o sns ses \3 sns usn ou osos soo sIn so sIus I nan naI .Ina onnn aov u smII ncoNaI u‘ o.moo~s 2 so I .ooowa w Ina no I n “Ina aaa anaa nao .saan IIu so xv I s.ooo~s OIoa aov u so xv I III m.eoo~s non IOanIono Ina oona aaa > aov u so aa .xaa I eons o sss «.ooons ssu so ose sss.gm.n se ose on oennss \3 esos soo n sss .so so I sss n.soo~s sssososs .nos .ssu > sss sass soo n .so soIs I . eons sonn gms. sns sesnIono sss sss s.~oo~s gms. .o.soo~s o n oes ssso .sos ssu usn sass ssso .soo n .so soIs I . «.soons sss sesnInuo .oos ssso so n \3 osos ssso .nuo s so .sss I 223 «a v.o~o~a ues n._ soo .so soIs I an «.omoma nInon Iaon so xv \3 Ina nna aaa aov .so vaI I : o.aaoua xaI aoanIsaan .Ina onnu nn van voa aOI n saan .aov so vaI I v.oao~a onnn w non Ina aaa > aa oonuaa \3 OIoa saan so vaI I o.aaona Ina aau oa OIoa aov xan I >nn non naI .sn.vao~av:m.~ nonn nan anaa aOI soa oa Avnaoaanauvvoa ssso so ou nse «ssu no> oes sass usn ou osos soo sss .so a osomsI . «.vaoua esos soo sss .so a I o.aaoma non aau Ina aan aov so I I so .aao m.nso~s .Ioo saan nao .nInon aaon aOI \3 voa soaIuvaOI saan .aov aaII .xan I ..o.~ao~a Ina aau sacn so vaI I o.aaoma onnu aOI aau saan so vaI I :m~.a n.aaona ones so so .sesnIono oases ssom mso sss gms. soo so so .sss I a.aao~a .oona nvaoaaa aau oa OIoa aov squn I I o.aaoos osos ssso n sss sso so sss .so eons o sss sss gm. “ssu usn sns sass soo n 5 .ns so ononsI sss s.s~o~s nan naI .aaa Ina anan aov u .so vaI I sss .ns. o.o~o~s nan .nInon aaon .voa u aov un .so vaI I sm.o~o~svgs ns m.o~o~s oso sou o sss use sneo .oos usn ou osos soo n .so soIs . I «.mmoos o oes use n use .soo sIn sss .ns s ononsI no I anon .Iunv von m.v~o~a unoo \3 oes “eons sues .sesnInuo .no a gm.s+ soo .nuo sIn sss .ns 3 I sns usn ou osos soo n soIns sIus «NousI nsnen sson ns .sss sumo m.n~o~s sonnn sa Ina aaon aaa > \3 OIoa :mo.~+ sIunv . n.n~o~a mason ssoo nso sss sneo oeo unoo oes ues gm.s+ soo n sss .so so I ssu sss soso snows "ssu so : > sss usn ou esos so I go+ noses ns 2 gm.s+ soo n soIs .ns s. snonsI sns ssu ou osos no n sss o.s~o~s o.s~o~s sosoos nos sessonoosos \3 sns ns no n gm~.s+ soo n sss .ns I sssovsoss ns “sneo oou unoo “.soIns usvoonn oenn sss uos soo n .so soIs ssonsI ns no a \3 o.aan onnn na Ina aaa aoanInao sso I onOI an n.ono~a svaaon w asan .nInon aaon sxaa nn> Ina anaa nao .aov IIu .so vaI I n.n~o~a -I .II ,>san n so so m IQNQNH as \flo flu , eons o seuss osos soo n so so snoosI uos sss oso o so gs+ sosos so a gs+ soo n sss .so so s.mno~s onnn na voa asan nao u sonnn w van Ioa na nav nInnn aaon xan “nan sIna aaa oona onnu aOI aov u ana .so xv mnoNaI onna w anI voa “.m.nso~svosoeo ssoo oso gm. “sns usn ou osos soo n. sns .so so «nossI voa maan nao u .Inov von anon .voaonmIoo voa saan .aov u ann .No I nnoNaI .I o.Nno~a sns usn ou osos soo n sns .so so I nINnoNa Inov von anon voaonIIoo voa aOI aov n so vaaa I n.~no~a nos .sos ssu oens soo n so squs s. I voa saan nao oIon “anon aao .xoa oona voa oaIn aov n soIHn I NnoNaI onns w nInon aaon sxanvIna aaa aan oa OIoa aov u squn I anomaI w.onoma onnn a nInon Iaon .sIvvoa .Inov von anon aOI aov u soIHn I I nnonoma onnn @ sxanvnInon aaon \3 DEC: aov a soIHn I I nInon aaon \3 voa n ssoo uos sesu sns no n .oos ssso so .seuss n ssso .soo sIn sss .so a onomsI w.o~oma seuss .oos so us on n > \o oses soo .sssn n so so I m.o~o~a Ina aan oa OIoa saan u so xv I 226 mason ssoo sss .~.seo~sIs.ooo~s sesn so .sss .~.seo~s Iaoo san .noa na on. 0a a: voa scan nao .aoaca scan .aov u .so vaI . I sesnIone nos “ssu noosos sass soo n so so osmosI n.mvo~a sesnInuo nuo a so so .so I u.mvo~a nInon aaon .aoaaa van OIoc Inaaaa aov u .so xv .u— n.ovo~a Ioo an scan saau aoaaa scan .aov u so xv _I_ n.noo~a ss.soo~svgm~.s sss sesnInuo .sos oens nuo .soo sIn ns .so a I scan .aco n.ovo~a sgs..ouoon ns .esne n so us I nnonn xaI aco “Iao nsn “voa scan “Ina onnu van aco .scan m.ovo~a sgm.s ou oooseuss ses susm .sesnIssso .seuss .nuo eIs so sIus I a.ovo~a coanInao .coanIscan .voa u scan .nao oII xanIso xv I nxnonn oona xac ano> \3 Ina aau > non .OIoc aon aov u so aaII ovowaI sssImo so m.ono~s anon naoon am von .soavaoaca .aOI .Ina Ion nao .aov a .so aaII I w.ono~a OIoc nao .aov II“ so aaII I so m.ono~s oao aoaannnaaoa «Ina saan nao .aov IIu aaII .xac I aca o.amoma. onnc o nInon aaon san scIn c3 scoanIaoo saoaaa scan .aov I so I I n.mmo~s cOanIaan sonnc w nInon aaon saoaaa aau nao .aov u so I I Iuov von aaon snInnn aaon anon saOI aov u no vaI mmoNaI. n.nmo~sg nan sIna aca oona aov IIu so vaI I an vcn voc xac n.nmo~a scan nao scOanIaoo scoanIaoa “saao>o avaoaaa scan .aov IIu .so vaI I_ xan o.amoua nInon aaon sonnc na voa scIn czInao oa saoo aau scan .aov IIu .so vaI I nInon aaon “Iao an scan c3 so.omo~avomo.~ xac o.amouafl scoanIaoo scoanIaon “snaan>n anno>onvaoaca scan .aov IIn .so vaI I n.omo~a o.avona w nInon aaon \3 OIoc aov u so I ..Im soo .sssn s.oeo~se .ssssoss .sos ssu > .sesnInuo .nuo n sss .so us I , osos soo n no so ooonsI voa scan csInao c3 .xac n.0voma, om~.a \3 nInon aaon ncv saoaannnnaoa oao I: scan .aov u .so xv I nInon aaon sac aoaaa n.oa snInon scan c3 .xac n.nvo~a ssoo so s.ooo~s o nnom so sssInoseuss .uos .nuo .soo sIn .so soIs .. I eue nos sessonoosos so.soo~s oss nos so.soo~s , w aOI snInon oaOan voa scan nao “Ina aca oona c3 .xac ~.n¢oNa_ oaaannnnon nInon aaon xac aca \3 ownn Ina aau scan .aov u .so vaI In E cc: sir.“ tc‘ul-w In... 1 g I ownn w mEnom ”Inaon nao 30H “aca n: v0: chanIaUaaam unbanIaoo aov . uao\ its g is: nao.mcan onnc o nInon aaon a.onona scoanIaoo «an onnu an scan nao svn .aoaaa IIu .aov OIu c3 .so xv I onnu n.onoma an scan nao_scoanIaoo «asan anon saoaaa aan scan .aov IIu so xv I . . aoo snInon scan o.anoma aaon anon svoc scan nao u “voa saoaaa IIu .nao .aov I an .so xv I I! nus n.onous esusness ns ssoo oso soo so so n > “on .seuss n nuo .soo s us .so so I onnc @ OIoc van nInon :aon \3 voa aau aoca Ina aca > aov u xac .so I nnonaI onnc o voa no I \3 nInnn aaon nav svaooc o.anoma o asan \3 Ina aOI aau sonnu nanocnon \3 OIoc aov u so I I «.unona aoaaa aau aov n so I I a.~wo~a voa aau oa OIoc aov u so I I onnc w nInon aaon “voa scan nao anon \3 xaI sccn ac .xac o.anoua oaaanoaI an san scan “asan saoaaa scOanIaoo .nao .aov IIu .so xv I sachnax "Ina aca oa OIoc aov m xac .mw I annual n.omons osn s.omo~s o ssun xac somoua sac oonu nnOI n.oa voa scan “Ina xca scan n.omoma 0a aOI “voa scan nao smm. oonuaa scoanIaOaaan .aov .nao IIu xac .so aa I eue nos o ssum “gm. nse ssso soIns o.omo~s voa scan oonuaa “ca I: aa aoo anon scOanIaoaaan .aov .nao I aa .so aa I onnc @ nInon . no ~.nmoma aaon sao 30m “Goa na voa scoanIaoaaan scoanIaoo aov .nao I Inc I .xac I _ cU‘c L: F"" o 1“ “I .‘ I all I." HII I g F . ~ I I . s I a - a Lx r . masdmm Caon anon «anon «amIU Forum—La nannao—a MN NUU .NOUK as; GAE V=U\ w.hwoNH\ 229 «.wooma sesnIsessso ssso .nuo sIn sss nInon aaon san swan c3 scOan nao .scan xac .c: Ianm sanno saoaao IIn Iov “Ina no u nIon \3 aOI .aov OIu .so vaI . nooNaI c3 I nInon aaon san sccn c3 scOanIaoo saoaaa I scan .Nao I .so vaI voowaI aco I m.noo~a_ use use “sesnIseo sseuss s .soo .nuo s sss I oes ssso sss masonsm oona c3Inao :m.a snInon aaon \3 Ina xca Iuov scan .aov u .so vaI . I, so o.asons sns nns non .sesnIsessso soo .suo sIn usIso .sss I . I osos soo n Iao s «somsIm n.aoo~a .s.sso~svgm.~ .sn.oso~svgm~.s uos «sss soso ssu soo n sss .so s I n.onoua. nInon Iaon “aoaaa u svn .coanIaoaaan aov .Nao I so aa .xac I_ n.onomam no I \3 an nan naI "no I van a o.aan Ina nao .aov IIu squc aaII I xac a.ono~a coanIaOaaan «Ina aca > soona no u an aoaaa aII aov .nao IIu .uc .so I I aco _ onnc na asan “voa aco n svn .coanIaOaaan .aov .nao IIu xacIso xv nnowaI, o.soo~s_ nInon aaon anon saoo sanno oonuaa saoaaa m nao .aov o c: .so xv I I III II. 4.“ \II- [at .W ICC hmEcwa CHO“ anon aoaca u aOE :m.n+ “asan voaUnQEOU an v0: so xv n ..n~.n+ “voa scan nso os .souss n .no I ..n.s+ sssn .so—e EIn .nn .xsn snow? a.nooNa OIoc aov u so vaI sns sass ssu stso n so so nooosI. OIoc aov u HoII ooonal scan v.ono~a_ sns snso ssu .use .soo n so soIs. I Inc onnn uos soo n so .sss ooomsI , ,No s.noo~s nos “sns snso n o soo n sIso .sss I sssn moooo~s_ sns snso ssu .use .soo n so soIs I OIoc aov u hquc I anomaI“ oao naa aoaannnaaoc “n.onoma a asan snInon aov .scan o.anoma I aaon anon saoo saoaaa IIu san van voa scan nao .nao IIu so Iva I nuo .sssn n.oso~s_ aoo san sccn “anno “voa aaav saoaaa IIu .aov IIu so xv . I nuo .sssn III s.oso~s_ aoaaa san scan c3 scoanIaoo scoanIaoa .aov I soIHn vaI I sssn m.ssonsw an scan c3 saoo sno aoaaan I anon svn aoaaa I .aov gnao IIu squc vaI II an scan .coan Iaoa aOI “no I anon \3 no u voa snInon aaon uneo seuss n uos gm.n+ sssum oeuenosee ns oes so so n gm~.n+ soes sssn nse os .seuss n .no I gm.s+ sssn .seo sIn .ns .sss ssomst asan van nEnmn ssoo unen «sou o gmm. sesnIone sss “go oss Iov OnOE .aEO sccn £3 chanIaOO saoaca acu Eln nav .sccn E xfih comma! 231 asan van nInon aaon anon .moa o smm. coanIono xac “so 3ac Iov onOI an scan c3 .coanIaoo .aoaaa aau IIu II“! nao .sccn sss momma! Appendi) gamgle FFZO FFZSa FF19 FF34 FF18 $811877 FF17 FP16 $811932 $811951 SBll951. FF24 FFZS $811959 FFlS FF29 rr14 FF13 5812095 3812108 rr12 FFll $812216 FF30 FF28 FF10 SB12393.4 S512395 FF23 FF32 FFg FPa 232 Appendix B--Brazos-Sun-Superior State Foster--Thin Sections samnls FF20 FFZSa FF19 FF34 FFlB $311877 FFl? FF16 $811932 $811951 SBll951.5 FF24 FF25 8811959 FF15 FF29 FF14 FF13 $812095 $812108 FF12 FF11 $812216 FF30 FF28 FF10 $312393.5 $812395 FF23 FF32 $812411 $812425 FF9 FF8 PF22 $812548 11674.5 11782.5 11786.6 11816.4 11844.6 11877.0 11881.6 11930.3 11932.0 i1951.o 11951.5 11955.5 11957.2 11959.0 11962.0 11994.0 12022.6 12087.3 12095.0 12108.0 12141.5 12213.6 12216.0 12245.3 12342.2 12343.0 12393.5 12395.0 12406.6 12411.0 12411.0 12425.0 12463.3 12520.2 12524.5 12548.0 Ds2§h_£&s .Bgsk_nams irregularly laminated micrite dol intrapelbiomicrite ls intraclastic sandstone silty intramicrite dol laminated micrite dol micrite dol ' siltstone to micrite dol micrite dol w/ siliciclastics bimodal silty micrite dol breccia- micrite, pelsparite, and fine to coarse crystalline dol, anhy cmt breccia- biolithite (stromlt), micrite dol, anhy cmt ' biopeloosparite dol silty micrite dol w/ anhy, chert cmt oobiomicrite dol laminated micrite and oosparite- dol sandstone, anhy cmt, anhy'nodules laminated micrite dol fine—grained anhy (fibrous) micrite dol silty biolithite dol sandstone, anhy cmt thinnly laminated micrite dol nodular anhydrite bimodal silty intramicrite dol breccia- biolithite, micrite dol, anhy cmt nodular anhydrite partially silicified biolithite (stromlt), anhy cmt laminated sandstone w/ anhy cmt irregularly laminated silty micrite and intramicrite dol intramicrite dol micrite to silty micrite dol pelmicrite to silty pelmicrite and thin lamination bimodal grainsparite micrite dol micrite to silty micrite dol laminated micrite dol and siltstone laminated micrite dol, oointrabiosparite ' bimodal FF7 SBlZSI FF33 FF27 FF6 FF26 $81264 $81265 $81265 $81266 $81267 $81269 881269 $812701 $812717 $812801 $812805 $812826 $812827 $812832 FFZl FFl FFZ $812879 $812897 FF3 5812924‘ $81294 FF4 l 8512961. FPS 8312982 $8129 89, 8812995 FF7 $812589 FF33 FF27 FF6 FF26 $812640 $812657 $812658 $812664 8812671 8812693 $312699 $812701 $812717 $812806 8812809 $312826. $812827. $812832 FF21 FF1 FFZ $312879 $812897 FF3 8812924.5 $312941 FF4 $312961.5 FPS $812982 $312989.2 $812996 ' 12563.5 12589.0 12593.1 12593.5 12620.0 12626.8 12640.0 12657.0 12658.0 12664.0 12671.0 12693.0 12699.0 12701.0 12717.0 12806.0 12809.0 12826.5 12827.6 12832.0 12834.0 12838.5 12860.0 12879.0 12897.0 12920.7 12924.5 12941.0 12948.1 12961.5_ 12969.7 12982.0 12989.2 12996.0 233 micrite dol oobiosparite dol bimodal sandstone w/ ool ite molds, intcl, micrite matrix dol micrite to silty micrite dol micrite dol to grainsparite (silt) intrapelmicrite dol sandy oomicrite ls, anhy cmt micrite dol to siltstone micrite dol to siltstone micrite dol, minor silt nodular anhy (intragrainmicrite) nodular anhy-(intragrainmicrite) laminated micrite dol to siltstone w/ pelloids, anhy cmt laminated micrite dol to siltstone micrite dol breccia thinnly laminated oosparite dol laminated micrite to silty micrite dol thickly laminated micrite to silty micrite and thin lam sandy ocpelsparite, anhy cmt laminated micrite, silty micrite, ocpelsparite, siltstone micrite to silty' micrite dol, anhy-rich laminated micrite and silty micrite dol, anhy-rich ' bimodally distr. sandstone w/ micrite bimodal sandstone w/ pelloids breccia- micrite dol, sandstone, silty micrite laminated bimodal sandstone w/ micrite and pelmicrite breccia- silty' micrite dol, pelsparite, anhy cmt intramicrite and micrite dol laminated micrite dol to siltstone biooosparite dol, minor sand, anhy cmt laminated micrite dol and siltstone I oosparite dol w/,anhy cmt micrite dol oosparite dol, minor anhy cmt c1assif: Irreguli Laminate Dolomite l. 0.02 to cement ( 2. material - P 968% Intrapeli Limeston. 55' 'c ' n Irregularly Laminated Micrite Dolomite 234 state roster rr 20 C s' dolomite anhydrite insoluble material pyrite quartz (‘IIII!I~ '% 1. Anhydrite and dolomite common, dolomite rhombs from 0.02 to 0.11 mm., burrows, cement (nonplanar to planar S) 2. Grain size appears to controlled by insoluble material, stylolite note dolomite appears to be a - Pyrite throughout thin section, approximately 2% ' ass' 'cat' Intrapelbiomicrite Limestone state Poster PP 25a a on o ' calcite anhydrite quartz K-feldspar pyrite insoluble material - Crinoids, Trilobites, Echinoderms 1. Fossiliferous, intraclastic, in various orientations, some anhydrite cement, pellets common V 2. Intraclastic, b3 so a- '\ ‘K ' \ \ coarse crystalline calcite cement common, fossiliferous, orientation of allochems generally more horizontal than 1. 3. Fossiliferous but much finer grained than above, pelloids very common, siliciclastics more common InI Sax tOI sanI app: intra 0f in fine- secti clast c0mm0 to in d°1omI 50min, 235 Stats roster PF 19 WWW PM Intraclastic quartz Sandstone microcline micrite (dolomite) anhydrite cement dolomite pyrite - Anhydrite throughout thin section 1. siliciclastic grains commonly 0.5 to 0.6 mm. (medium to coarse sand size), subrounded, approximately 35%, dolomite, anhydrite, dolomite micrite 64%, pyrite 1% 2. Less dominant siliciclastic area (approx. 5% of the sand size grains), dolomite micrite common, some rhombs of approximately 0.04 mm. - Intraclastic - Possibly some anhydrite-filled molds State roster rt 34 s“- 1° a .0 H'e 1).. : 0 0O on ‘o, Silty Intramicrite dolomite Dolomite quartz K-feldspar insoluble material anhydrite O 1. Intraclastic, (fine) polymodal planar S to E dolomite intraclasts, insoluble material commonly concentrated at edges of intraclasts, commonly greater than 1 mm., they appear very fine-grained and buff to the naked eye, occur throughout thin section; sandy 30%, grains commonly part of matrix around clasts but. also appear ‘within. some. of the intraclasts, commonly 0.4 mm.: dolomite matrix appears to be very similar to intraclasts described above --> (fine).polymodal S to E dolomite 2. Dolomite becomes polymodal planar E, solution seams dominant, siliciclastics less common 3% and much finer 0.05 mm. C 8551 Lamina Dolomi well 2 some p and ma M Micrit 236 Stats roster rt 18 85' ' 'e 05' 'n Pastures Laminated Micrite dolomite Dolomite pyrite anhydrite cement, nod. L quartz plagioclase microcline \fi/ 1. Anhydrite cement 65%, siliciclastics 35%, rounded to well rounded, approximately 0. 4 mm. (medium sand size). in some places anhydrite is in nodules: PYrite less than 1% 2. Interlaminated areas of material less than 0.01 mm. and material with siliciclastics as large as 0.02 mm. State roster, 8811877 .ss',' a f- iI- : o-° z o ..s' “-I ~. - -s Micrite Dolomite dolomite quartz anhydrite -minor pyrite insoluble material plagioclase -trace microcline -trace - Dolomite is generally bimodal planar S, the larger mode dolomite appears to be fracture related or in clasts 1. Solution seams that contain a higher percentage of quartz than the rest of the thin section 2. Areas of more coarsely crystalline dolomite, sizes approximately 0.1 mm. 3. Areas of finer crystalline dolomite, sizes approximately 0. 05 mm. 4. Concentration of insoluble material (again higher % of siliciclastics):.some silica cement in spots near solution seams as well as some minor anhydrite cement - Almost purely dolomite with areas of coarser crystalline dolomite that appear to be intraclasts possibly - Minor silica and anhydrite cement (possibly a late stage cement) glass}! siltstc Dolomit 1. must be approxi‘ 2. 3. approxit 4. Commonlj 5. 4. mate} burroweI Micrite ”4th Bi: SlliCic: 237 State roster It 17 Wmfim PM Siltstone to micrite quartz Dolomite dolomite anhydrite nod, cmt [::::::::j pyrite insoluble material microcline ; pleochroic grn -rare 2 1. - Darker very fine area (less than 0.01 mm.) minerals must be oriented due to unity of extinction -Lighter interlaminated areas: siliciclastics at approximately 40% and 0.06 mm. (coarse silt) 2. Anhydrite nodules common as well as anhydrite cement 3. Anhydrite nodules present as well as siliciclastics at approximately 50% and 0.04 mm. subrounded 4. Anhydrite nodules and cement dominant, siliciclastics commonly 0.05 mm. 5. Darker very fine area like 1. but contains clasts of 4. material without the anhydrite nodules, note: this appears burrowed, dolomite and anhydrite cement State Poster P! 16 s'_' a_io I°Ie,a --' -, C-m-osi ,O! -. -s Micrite Dolomite dolomite with Bimodal quartz —- Siliciclastics I anhydrite fl pyrite I 2 plagioclase { ; “ muscovite -trace insoluble material - Distinctly bimodal siliciclastic distribution: larger grains approximately 0.65 mm. (coarse sand size), finer grains approximately 0.03 mm. (coarse silt size): subangular to subrounded . 1. - In area where thin section is quite thin dominant anhydrite cement becomes quite apparent: in this area siliciclastics make up approximately 50% of the sample, pyrite can be seen throughout this area at approximately 1% - Areas with insoluble material contain less siliciclastic material at approximately 25% 2. larger siliciclastics more. dominant in these laminations, dolomite matrix, pyrite somewhat larger here‘: note 1 silic1i silic1< 3. to are dolom11 4. glassiz Bimodal Dolomit here, c bimodal 3% coax dolomitI Silicicj Silicic; QEEEELQA BreCCia. Pelspar; ° CoarI DolomitI Cement NH! PYrite" appear; Silicic' note larger siliciclastics gggnded to subrounded, smaller siliclastics subrounded to subangular: 21.820.81.121 of siliciclastics distinct here 3. Siliciclastics approximately 40%, grain size 0.02 mm. to areas with approximately 30% and grain size 0.01 mm., dolomite cement 4. Insoluble material 8tata roster, 8811932 W108 ‘ Fm Bimodal Silty Micrite dolomite Dolomite quartz ‘ $3 K-feldspar pyrite 2 insoluble material mica ~ 1. Coarser quartz and orthoclase grains concentrated here, 0.4 to 0.5 mm., less solution seams here, definite bimodal siliciclastics, finer portion 0.02 to 0.03 mm. 3% coarser’ siliciclastics, 40% finer' siliciclastics, 55% dolomite, 2% pyrite 2. Similar' to 1. 'with 'the absence of’ the coarser siliciclastic fraction and an increase in solution seams 3. Possibly a burrow, note higher percentage of siliciclastics State Poster, 8811951 glasgifigatign mineralogical Composition Breccia- micrite, dolomite Pelsparite, and Fine anhydrite to Coarse Crystalline pyrite Dolomite, Anhydrite quartz Cement - Breccia 1. Stylolite seperating sections 2. and 3. . ‘ 2. Dolomite micrite with anhydrite filled fractures, pyrite throughout, bimodal 3. Coarser nonplanar dolomite approximately 0. 06 mm., appears cross-bedded 98% dolomite, 1% pyrite, 1% siliciclastics 239 4. Hicrite (possibly dolomite) contains fine pyrite crystals, micrite somewhat coarser than 2. but finer than 3. 5. Coarser than 4. nonplanar dolomite 6. Fracture filled with anhydrite terminates at stylolite State Poster, 8811951.5 Won Pastures Breccia- Biolithite anhydrite (stromlt), micrite dolomite Dolomite, Anhydrite pyrite 2 Cement insoluble material a L _ 13 - Stromatolite breccia 1. 100% anhydrite cement 2. Silt size material approximately 0.02 mm., appears to be dolomite permeated with anhydrite cement: pyrite throughout at approximately 1%: insoluble material present,: siliciclastics present 3. Material similar to 2. except areas have higher concentrations of pyrite or more coarser crystalline dolomite (0.13 mm.) also areas with greater concentrations of anhydrite cement state Poster 88 24 lass fica 'on n a o i a on s't n . Egaturgg Biopelsparite Dolomite dolomite anhydrite fié755’: /”’ quartz chert ’55??? insoluble material 1. Stromatolite or algal laminations, dolomitized a. anhydrite and chert cement ' 2. Dolomitized oolites (some squished), Brachiopods, Crinoid fragments: scattered siliciclastics 3%: Brachiopods generally oriented with crystalline dolomite beneath: clear fleck's throughout are anhydrite cement, appear as dark fleck's in hand sample: matrix dolomite micrite and polymodal A to S dolomite ' 240 Btltl roster PF 25 :1 'E' !° H' J . J E .!. n F ! Silty micrite Dolomite dolomite with Anhydrite and anhydrite Chert Cement chert quartz insoluble material 1. Micrite to fine crystalline dolomite with subangular to subrounded siliciclastics 2. Anhydrite cement 3. Dolomite cement, silica cement, anhydrite cement, micrite present - 8tatn roster 8811959 Classification fligegglggigal Composition Features 00biomicrite Dolomite dolomite 2 anhydrite cement insoluble material pyrite quartz muscovite -rare plagioclase microcline " l - 95% polymodal nonplanar dolomite, 1% siliciclastics, 4% anhydrite cement and insoluble material 1. Anhydrtie cement 100% 2. Possibly dolomitized Echinoderm fragments - Anhydrite cement often associated with organic material: both appear to be filling fractures 3. insoluble (organic) material, contains mainly siliciclastics (subangular) - Coarser crystalline dolomite areas probably burrows, vague ghosts of oncolites or oolites 241 8tatn roster It 15 WWW PM Laminated Micrite dolomite ‘ I and Oosparite Dolomite pyrite anhydrite 2 quartz plagioclase , muscovite -trace a 4 a 1. Abundant insoluble material, siliciclastics at approximately 0.1 mm. (very fine sand size), some anhydrite cement, minor pyrite: interlaminated with areas with dominantly dolomite matrix and approximately 5% siliciclastics of very fine sand size 2. Material is dominantly less than 0.01 mm.: appears to contain anhydrite throughout, dolomite, and approximately 5% siliciclastics, also minor pyrite present 2. and 3. are quite similar but the boundary seems very distinct 3. Transition to a slightly coarser area with somewhat more dominant anhydrite (some small nodules) and possibly more abundant siliciclastics (some as large as 0.1 mm.) 4. Squished ooids, ooids dissolved later filled with anhydrite cement, some still have dolomite or calcite in their centers: grains are well rounded, average approximately 0.15 mm. (fine sand size), dolomitic micrite coating grains 8tate Foster 88 29 lassi 'cat'on ' era ' a1 om 5 ion Fegggggg Sandstone, Anhydrite quartz Cement and Nodules microcline plagioclase anhydrite chert dolomite insoluble material 1. Chert clast containing some anhydrite 2. Anhydrite rim 1. and 2. --> silicified nodule 3. Sandstone with anhydrite cement, grains to 0.9mm 4. Anhydrite nodules! 5. Sandstone with anhydrite nodules common, dolomite micrite matrix, insoluble material -a> SOlution seams 242 8tatn roster P! 14 S. ' g. 0: v19: 0,: -. OLO- ' ,0! Laminated Micrite dolomite micrite n... Dolomite anhydritecement r‘*’// quartz plagioclase microcline orthoclase pyrite %‘ 1. Material in these areas is medium silt size at approximately 0.02 mm. and less, 97% dolomite silt, 25 pyrite, 1% siliciclastics: areas which generally trend horizontally across section, slightly coarser dolomite at approximately 0.02 mm., often contain insoluble material, anhydrite cement, possibly some burrows 2. ‘ 3. Lateral cracks cemented by anhydrite, burrows, a. insoluble material in very fine (silt size) areas often interlaminated with b. material similar to that described in area 1. above . - Some areas also contain anhydrite nodules also some laminations have a higher percentage of siliciclastics - Pyrite found throughout thin section state Poster PF 13 glaosifiioaoioo ninegologioo; Qomoosigion Eooooxoo Fine-grained Anhydrite anhydrite pyrite quartz plagioclase insoluble material _J - Burrowed - Anhydrite permeating throughout thin section 1. Siliciclastics and pyrite concentrated here: pyrite relatively coarse at 1.1 mm., siliciclastics at 0.1 mm. ~ 2. Pervasive anhydrite, algal laminations, siliciclastics O. 02 to 0.10 mm. ' - Thin section appears to be quite burrowed, relatively. homogeneous: two laminations where siliciclastics more abundant and large pyrite crystals concentrated 243 Stat. FOItOr 8812095 Wicn Peasants: Micrite Dolomite dolomite pyrite siliciclastics - Homogeneous micrite ‘with. minor siliciclastics at approximately 0.02 mm. and less than 1% - Pyrite throughout thin section - One small area of section shows abundant siliciclastics at 0.1 mm., rounded: anhydrite cement: insoluble material State roster 8812108 oowwn Beanies Silty Biolithite dolomite ‘ ' Dolomite quartz 2 plagioclase pyrite muscovite -rare I anhydrite cement insoluble material anhydrite 1. Grain size generally < 0.02 mm., relatively homogeneous, siliciclastics 1%, some clusters of coarser crystalline dolomite possibly a replacement texture 2. As approach 2. from 1. note increase in insoluble material, siliciclastics and overall grain size, minor anhydrite cement present in areas - Siliciclastics 7%, 0.05 mm. - Fractures crossing laminations are filled with anhydrite - Interlaminated finer and coarser (<0.01 mm. and approximately 0.02 mm.) material 8tatn Poster rt 12 Win PM Sandstone, Anhydrite quartz Cement anhydrite cement microcline orthoclase pyrite silica cement . dolomite 244 - Siliciclastics dominate thin section with two very fine laminations containing dolomite micrite are apparent 1. Dolomite dominated micrite matrix (polymodal planar -S to -E dolomite) in a thin lamination: very fine grained pyrite in areas: some areas with slightly coarser dolomite on the order of 0. 02 mm. 2. Similar to 1. but has pore space 3. Siliciclastic grains 0.3 to 0.5 mm. well rounded to subrounded: dominant anhydrite cement: some grains showing replacement textures: 72% siliciclastics, 10% anhydrite cement, 5% silica cement, 2% dolomite, 1% pyrite 8tatn Poster PP 11 glossigicotion ninezologiool ooooooition FIQLQIIE Thinnly Laminated dolomite micrite Micrite Dolomite anhydrite illite - possibly pyrite some silica cement J 1. Anhydrite modules that lie along a lamination 2. Minerals oriented with possibly insoluble material (also oriented) slump structure 3. Possibly a burrow, appears to have a higher percentage of anhydrite or illite 4. Pyrite crystals 0.6 mm. - Dominantly micritic size material with a high percentage of either anhydrite or illite: anhydrite nodules are present. Alternating light and dark laminations appear to reflect the amount of insoluble material present 8tatn Poster 8812216 Widen Features Nodular Anhydrite anhydrite, dolomite quartz K-feldspars insoluble material - Anhydrite nodules, rounded, 90% - Matrix material, 10%, permeated with anhydrite - Polymodal nonplanar dolomite commonly 0.1 mm. in size, 85% of ‘matrix ‘material, 10% anhydrite cement, 5% siliciclastics - Dolomite appears corroded 245 _ state Poster PP 30 Won Features Bimodal Silty dolomite Intramicrite Dolomite quartz chert -minor, detrital K-feldspar anhydrite -minor insoluble material - Soft sediment deformation - Mottled areas mixture of dolomite micrite dominated areas and siliciclastic-rich areas that are commonly bimodal and subangular to subrounded - Some solution seams 8tste Poster PP 28 5' ° -. 0! III‘ o. 9062,, “I00 0! Breccia- Biolithite, dolomite Micrite Dolomite, anhydrite Anhydrite Cement insoluble material quartz -minor pyrite 1. Anhydrite cement (fibrous crystals) 2. Dolomite micrite a) to fine anhydrite crystals 3. polymodal S dolomite, crystals surrounded by insoluble material: anhydrite cement in areas 4. Algal: algal laminations 5. molds filled with anhydrite cement: dolomite in center of some of the molds possibly a second cementation: not just dolomite sitting on top of anhydrite: boundaries of molds surrounded by insoluble material: possibly oolite molds: also dolomite fossil fragments possibly present 246 8tate Poster PP 10 Qlaasifisati2n______uinsralogisal_£2messition greatures Nodular Anhydrite anhydrite' dolomite I quartz 2 illite pyrite 2 plagioclase -trace w - Dolomite grains average size 0.12 mm. 1. Clast of finer dolomite grains (grain size average 0.03 to 0.05 mm.) - Micritic areas (possibly containing dolomite, anhydrite, illite) between larger dolomite grains --> discontinuous areas of finer grained dolomite ' 2. Anhydrite nodule - Relatively homogeneous, no major compositional changes or structural changes within the thin section. Dolomite may be described as bimodal planar S, either detrital or being replaced by anhydrite state Poster 8812393.5 _.ss' 'c. :01 I' e.a o-i - Ou°° 5 5- -1 -s Partially silicified anhydrite ‘ F—--==- Biolithite (stromlt), pyrite Jn.L——sfl Anhydrite Cement insoluble material I 2 quartz l dolomite plagioclase LA l. Bimodal siliciclastic grains dominate, rounded to well rounded, commonly 0.5 mm. (medium to coarse sand size) or 0.05 mm. (silt size): anhydrite cement and insoluble material present here also micritic material: a. 50% siliciclastics, 0. 02 mm. (silt): I think anhydrite cement: pyrite‘throughout approximately 2%: b. laminations containing both sizes of siliciclastics but different matrix: laminations alternate between a dominant micrite matrix and a matrix with a higher % of the finer siliciclastic fraction.and insoluble material: note pyrite throughout ' ' 2. Anhydrite and chert: pyrite common, burrowed --> MostLy chert anhydrite replaces chert: possibly a second stage of chert after anhydrite but not likely 247 --> Stromatolite irregulary replaced by both anhydrite and chert giving it a mottled appearance 8tate Poster 8812395 0 o! y g‘ ‘1 e2 0”... I] ‘;_ _ ‘- Laminated Sandstone anhydrite with Anhydrite Cement quartz h dolomite microcline orthoclase pyrite 1. Laminations 1. bimodal siliciclastics (0.25 and 0.03 mm.) , rounded: anhydrite cement: pyrite: 2. micrite, insoluble residue dominated finer siliciclastic fraction, pyrite: 3. coarser siliciclastic fraction with anhydrite cement: 1.: 3. 2. Similar to 3. described above, siliciclastics 0.45 mm. well-rounded: anhydrite cement 3. Dolomite (micrite) matrix 70%, 0.01 mm.: siliciclastics rounded to wel rounded 30%, 0.35 mm. - Some feldspar cement replacing anhydrite 8tate Poster PP 23 Widen features Irregularly Laminated dolomite Silty Micrite and chlorite Intramicrite Dolomite‘ pyrite quartz .S_\\’J_\\ K-feldspar 2~a—s\,_ anhydrite (minor) '*—*~*-- insoluble material "TPJss—L/P - Mottled to very irregularly laminated 1. (lighter areas) siliciclastic-rich 85% subangular to subrounded: anhydrite and minor chlorite, pyrite and insoluble material as a matrix 2. (darker areas) finer grained, less siliciclastics than 1. and finer grained, chlorite-rich, fine-grained pyrite throughout 3. I intraclast, generally like -2, darker possibly due to presence of more insoluble material or disseminated pyrite " 248 State Poster PP 32 _a s i 01.. 4.19 -, 0A3 ,- euee e! Intramicrite Dolomite dolomite quartz A .—/"'~ \ anhydrite l<;;§;;;> muscovite lac’fgggg 1. Crusts, 2. 70% dolomite micrite to fine crystalline anhedral: anhydrite and siliciclastics common: note quartz and dolomite commonly‘ the same size: detrital dolomite?: alsoI cross- laminations a. 8tate Poster 8812411 Waco PM Micrite to Silty dolomite Micrite Dolomite pyrite siliciclastics - Siltstone - Siliciclastics of the 0.03 mm. fraction ‘make 'up approximately 5% of the thin section 8tate Poster 8812425 C ass' 'ca '0 ' r o ' cm '0 Pelmicrite to Silty dolomite Pelmicrite and Thin quartz Lamination Bimodal plagioclase Grainsparite muscovite orthoclase muscovite anhydrite pelloidal‘micrite insoluble material 1. Cross-laminations alternating laminations of a higher % siliciclastics (25%) and a lower % of siliciclastics, mainly micrite, commonly pelloidal micrite: opaque material present throughout --> organics: siliciclastics commonly 0.07 mm. subangular 2. Coarser crystalline dolomite filling in fracture, note - appears to be microfaulted 3. Opaque material --> organics (?) 249 4. Siltstone: 7% siliciclastics 0.03 mm. subrounded to subangular: dolomite becomes relatively coarse crystalline in "pockets or nodules": organic material present , 5. Coarse grained siliciclastics here 0.5 mm. well rounded, also appears to be dolomite replacement of fossil material, one appears to be an echinoderm fragment, rare anhydrite present ‘ 6. Burrow (7) filled with material similar to 7) 7. Siliciclastics with dolomite and anhydrite matrix, bimodal (0.45 and 0.05 mm.), insoluble material present 8tate Poster PP 9 Wu Featurss Micrite Dolomite dolomite chlorite apatite pyrite 1. Burrow 2. Soft sediment deformation - Possibly anhydrite (lath shaped) throughout - Containing chlorite? throughout, pleochroic 8tate Poster 2? 8 Qlossificaoion ninezologioal gomoosigion Eoogozoo. Micrite to Silty dolomite Micrite Dolomite quartz “—-~._\~_‘~ pyrite 3 muscovite 2 anhydrite plagioclase probably orthoclase - Solution seams 1. Clumps of anhydrite, quartz, plagioclase, etc. 0.02 mm.: material finer than area 2. possibly burrOw fills or rip- up clasts 2. Anhydrite cement throughout: insoluble material or organics common 3. Darker (high organics): bands with higher quartz content containing some anhydrite or dolomite cement - bands pinch-out in areas but generally continuous across section: 250 elongate minerals aligned - Silt size siliciclastics common in areas with less insoluble material 8tate Poster PP 22 0 O 0 :ss . o I I- g u: . ou-o- oI Laminated Micrite dolomite Dolomite and Siltstone quartz K-feldspar muscovite r_. chlorite l 7" anhydrite (minor) ' insoluble material t::::z:::j’ - Laminated (regular, thin) 1. Chlorite-rich 80% oriented horizontally, siliciclastics 17% very fine grained, pyrite, etc. 3% (very fine grained) 2. Siliciclastic-rich up to 90% coarsening upward also becomes progressively less chlorite-rich, fine laminations of pyrite crystals 0.1 mm.: siliciclastics generally subangular elongate minerals oriented in various directions 3. Like 1. only more insoluble material present 8tate Poster 8812548 Qlosoifioogion flinozologiool Qomposigion Fooggroo Laminated Micrite dolomite 2 Dolomite, anhydrite ‘3, Oointrabiosparite quartz a - Trilobite hash . 1. Dolomite micrite, rare quartz 2. Coarser dolomite filling fractures? replaced fossils? (oncolite) burrows some anhydrite some siliciclastics 3. Oolites and other replaced fossil fragments with micrite outlines: coarser dolomite than 1.: nonplanar to planar S dolomite cement: intraclasts ‘ 251 8tate Poster PP 7 -SS.,: . .0! 2.0‘ . so { c.1908. .0! "z A ’S Micrite Dolomite dolomite quartz muscovite plagioclase anhydrite -minor chert -trace - Solution seams - Nonplanar to planar S dolomite - Grain size approximately 0.04 mm. 1. Crack filled with late stage polymodal planar S dolomite cement also some anhydrite cement - A few small laths of anhydrite 8tate Poster 8812589 C 55' 'c tio 'ne a ' a 0 ion IFoooozoo 1 Oobiosparite Dolomite dolomite anhydrite l silica cement % quartz ii - Oolites, echinoderms ghosts 1. Possibly anhyfrite nodules, much coarser dolomite rimming these areas 2. Finer grained dolomite nonplanar with rare siliciclastics and anhydrite: note oolite and fossil or other ghosts are not as common in the finer grained areas 3. Coarser crystalline dolomite with frequent oolite and- other ghosts dolomite ' is polymodal nonplanar to planar S, anhydrite cement common, minor quartz generally subrounded to rounded 252 8tate Poster PP 33 s ' 'c t o ' ° ' n FEQSQIEfi Bimodal Sandstone quartz with Oolite Molds, dolomite Intraclasts, Micrite anhydrite Dolomite Matrix chert -minor K-feldspar -minor 1. Intraclasts, generally composed of dolomite micrite with minor anhydrite and quartz, some clasts appear to be squished ‘ 2. Quartz-rich 55%, rounded, commonLy 0.5 mm.: matrix dolomite micrite: rounded areas common that appear to have had something dissolved out and was later filled with anhydrite cement <-- fibrous radiating crystals (dissolved ooids?, very rounded) - 8tate Poster PP 27 Wig—KWEn Pastures Micrite to Silty dolomite . Micrite Dolomite anhydrite quartz K-feldspar 1E5?— plagioclase -minor pyrite -minor muscovite -minor l. Dolomite micrite, faint very thin laminations a. are alternating with dolomite micrite to fine anhedral dolomite and more siliciclastic-rich 10 to 15%, subangular to subrounded, 0.05 mm. 2. 25 to 30% siliciclastics, bimodal, subrounded to subangular, 0.4 to 0.04 mm.: matrix dominantly dolomite micrite to fine crystalline anhedral dolomite, some anhydrite cement 8tate r8822: PP 6 O O O O S -_ S ,- 0! II 1‘ -. .A! o, sus- °l Micrite Dolomite dolomite to Grainsparite (silt) quartz microcline anhydrite muscovite plagioclase 1. Dolomite unimodal, growth appears to have been controlled by presence of insoluble residue - Anhydrite is present but not pervasive as cement in elastic areas 2. Mudcrack filled with material from 3. 3. Contains a variety of minerals (listed above) average grain size 0.07 mm. 4. Stylolites or solution seams 8tate Poster PP 26 ogassificaoiog ninozologiool oomoooigion Foogozoo Intrapelmicrite dolomite I Dolomite anhydrite quartz ‘. insoluble material 1. Large intraclasts of fine unimodal anhedral dolomite to dolomite micrite 2. Dolomite micrite intraclasts rounded: .matrix is a coarser crystalline polymodal A to S dolomite with some siliciclastics 2% and intraclasts: some anhydrite 254 State Poster SS12640 -SSi ' - OJ .iIe 1 9° 1 Ono-S :0! e. ‘5 Sandy Comicrite dolomite Limestone, Anhydrite calcite Cement chert quartz anhydrite intraclasts insoluble material - Squished oolites, with solution seams surrounding them, some oolites dolomitized: coarse siliciclastic grains also surrounded by solution seams - Anhydrite filling in some areas where oolites have been dissolved out 8tate Poster 8812657 ass' ’ca 'o ° ° a s 'on Foooogoo Micrite Dolomite dolomite to Siltstone quartz microcline anhydrite insoluble material - Mottled laminae alternating silt and dolomite micrite - Insoluble material common throughout 8tate Poster 8812658 .ss' 'ca '0 'I- . --7ca_ . oos' 'o -;t Micrite Dolomite dolomite to Siltstone quartz microcline plagioclase anhydrite - Siltstone - Fine siliciclastics in dolomite micrite matrix 8tate Poster 8812664 glassifioaoion Minoxglogiool Qomoosigion Foooozoo Micrite Dolomite, dolomite ’ Minor Silt quartz microcline plagioclase . anhydrite -minor - Planar E to planar S dolomite - Bimodal siliciclastics larger grains rounded 255 State Poster 8812671 0 e 0 e e S . 0! v I‘ t “A E 01190 9,! Nodular Anhydrite anhydrite ' (Intragrain-micrite) silica cement quartz I insoluble material orthoclase :EEE?' plagioclase ‘ 2 / m 1. Silica with euhedral to subhedral crystals of anhydrite 2. Anhydrite more dominant than 1. with nodules of silica ? being replaced by anhydrite? 3. Anhydrite nodules in solution seams, scattered siliciclastics 4. Same as 3. State Poster 8812693 a ,' ' a '-I I'I- g -- ., cu-o ' '-I -= _ -s Nodular Anhydrite anhydrite (Intragrain-micrite) dolomite siliciclastics 1. Anhydrite nodules some areas with insoluble material (brown) filling in around nodules often containing siliciclastics 2. Insoluble material more common - Infrequent coarser crystalline planar= S dolomite "nodules" within anhydrite nodule ' 8tate ran??? 8812699 glgsgifiigatign _ Hingzglggiggl ggmpggition LFggggzgg Laminated Micrite dolomite Dolomite to siltstone quartz with Pelloids, anhydrite Anhydrite Cement microcline plagioclase - Laminated possibly low' angle cross-laminated alternating dolomite micrite and dolomite micrite with siliciclastics - Note anhydrite common as cement and fracture fill 8tate roster 8812701 -5 .' t 01 v.1' ._ 0g . 0120- 01' '-, S Laminated Micrite dolomite Dolomite to Siltstone quartz microcline anhydrite insoluble material - Laminated siltstone, note thin coarser grained laminae, containing microcline, quartz, anhydrite, also micritic intraclasts with concentric micritic rings in this coarser laminae --> dominantly anhydrite with silt sized siliciclastics 8tate tostar 8812717 Classification Mineralggiggl QQEQOSigiQn Featgrgg Micrite Dolomite dolomite I anhydrite - Siltstone, dominantly anhydrite and insoluble material 8tate roster 8812806 Qlassifi2atiQn______Mineralogical_99m22§itign Features Breccia dolomite anhydrite silica cement insoluble material feldspar cement - Breccia 1. Feldspar grain being replaced by anhydrite? “257 2. Polymodal nonplanar to planar's dolomite and dolomite micrite; burrows especially horizontal burrow at base: fractures filled with insoluble material containing anhydrite nodules as well as some dolomite 3. Anhydrite filled fracture 4. 5. Anhydrite and coarser crystalline, note lower boundary micritic with scalloped appearance along fracture 6. Mottled: algal laminations; insoluble material containing dolomite siliciclastics, silica cement, anhydrite cement; anhydrite laths 8tate roster 8812809 .8 ° ° at'o v.1‘ 1 -- 1 ouo-r o; “:e Thinnly Laminated dolomite 2 ‘ Oosparite Dolomite anhydrite orthoclase ' - Replaced oolites in dolomite and anhydrite cement also feldspar cement? 1. Intraclast also containing oolites 2. silicified oolites - Note dogtoothed dolomite cement with possibly later stage silica cement - Detrital siliciclastics - Commonly coarser crystalline dolomite cores of oolites 8tate roster 8812826.5 Widen PM Laminated Micrite dolomite to Silty Micrite quartz Dolomite anhydrite 1 microcline insoluble material 1. Higher in insoluble material 2. Less insoluble material 3. Fractures filled with anhydrite, siliciclastics 258 8tate roster 8812827.6 Wion Features Thickly Laminated dolomite Micrite to Silty quartz ' 3 '77 Micrite and Thin anhydrite Laminated Sandy plagioclase 2 Oopelsparite, insoluble material , , L Anhydrite Cement ‘r“\_;57 1. Higher in insoluble material, siliciclastics, dolomite micrite, burrowed 2. Very high in anhydrite, gradually increasing in insoluble material as move up from boundary with 1. also increase in siliciclastics 3. Anhydrite cement, detrital siliciclastics, dolomite micrite, pelloids, some siliciclastic grains have micritic envelopes, intraclastic 8tate roster 8812832 WWEn Laminated Micrite, dolomite Silty Micrite, anhydrite Oopelsparite, Siltstone pyrite quartz plagioclase microcline muscovite 1. Siliciclastic-rich 2. Finer grained, burrows filled with siliciclastics, ?altered areas?, siliciclastic laminae at the top»of this area 3. Dolomite micrite, oolites, scattered siliciclastics, anhydrite cement in areas: often coarser crystalline.dolomite cores with micritic envelopes 4. Dolomite micrite, some anhydrite cement (or nodules with dolomite micrite) 259 8tate roster rt 21 a. so 0 at. I O O 8 O n PM Micrite to Silty dolomite Micrite Dolomite, anhydrite Anhydrite-Rich chlorite 1 pyrite quartz :::: plagioclase ‘ 1 insoluble material - -_1,. -.__.——-__‘ “fllllll!=!' 1. Chlorite-rich 40%, fine-grained siliciclastics 35% subangular, pyrite, etc. 25%; elongate minerals oriented long-axis horizontal - 2. Irregularly laminated; a. dominantly quartz and anhydrite, less chlorite than 1., larger grains of pyrite, concentrated insoluble material: b. nodules containing anhydrite and siliciclastics (50:50) oriented along laminations: areas around nodules like 1.: c. ? fracture (horiz) filled with silica cement ? 8tate Poster 22 1 f.ss' 'ca 'oz vine - ..' a_ . 90 ' .. ”a _ -- Laminated Micrite and dolomite Silty Micrite Dolomite, anhydrite Anhydrite-Rich quartz f 3 5 ': microcline -trace 1r—-———\__l orthoclase ‘ I plagioclase __ 1 pyrite I 3 7 biotite -trace ' chlorite -rare l. Mudcrack filled with anhydrite 2. Grain size larger, average size of feldspars and quartz 0.3 mm: some dolomite cement . 3. Interlaminated areas of very fine material (micrite) with somewhat coarser areas, but still fine grain size; pyrite throughout 4. Coarser grains (up to .25 mm.) higher anhydrite content: solution seams; uneven surface (contact.between'very fine grained 3) and coarser grained.area): many features look like compaction features; areas look like clasts ,of siliciclastic materials or anhydrite (both coarser and very fine grained) - anhydrite nodule 5. Lose solution seams 6. Fine grained, solution seams, nodules 7. Grains coarser related to 6.: (remnant of _ 260 underlying bed) 8tate roster Pr 2 8 0 O o O '5 . 'l y 1‘ . 0° jo, 01100, 0! Bimodally Distributed quartz Sandstone with Micrite plagioclase orthoclase dolomite matrix anhydrite cement microcline -trace chert -trace - In pore spaces dolomite rhombs become somewhat larger - Dolomite matrix may be beginning to replace quartz - Quartz 0.15 mm., subangular, undulose extinction 1. Dolomite fragment surrounded by anhydrite cement 2. Anhydrite and dolomite cement replacing quartz: quartz is 0.25 to 0.35 mm. , subrounded to rounded, straight and undulose extinction: larger grains often clumped together in a mass cemented with anhydrite 3. Band of material (quartz); in other areas this material appears to fill in cracks - Bimodally distributed sandstone in a very fine crystalline dolomite matrix with poikioltopic anhydrite, note: poikioltopic anhydrite mostly associated with coarser grained areas 8tate roster 8812879 Classification. ningzalggigal 99mposition - Features Bimodally Distributed dolomite Sandstone with Pelloids quartz microcline anhydrite l. Intraclast (fossil replaced with dolomite micrite?) - Matrix dolomite micrite to polymodal nOnplanar dolomite (in general) . ' - Detrital. quartz, subrounded to well rounded, note commonly strained to polygonal - , - Some anhydrite cement 261 8tate roster 8812897 :1 'E' !i ll' 1']: “in Breccia- Micrite dolomite Dolomite, Sandstone, anhydrite Silty Micrite quartz muscovite collophane microcline - Matrix dolomite micrite, coarser dolomite in fractures 1. Dolomite micrite with scattered fine siliciclastics 2. Algal laminations ? 3. Dolomite micrite matrix, bimodal siliciclastics larger grains rounded to well rounded, replacement at edges of grains by matrix material 4. Insoluble material with abundant siliciclastics and some anhydrite 8tate roster rr 3 :1 s .E. !° H' J i 1 E o .!. n .F ! Laminated Bimodal dolomite Sandstone with Micrite quartz and Pelmicrite Dolomite pyrite anhydrite chert microcline -rare plagioclase chlorite -rare biotite 1. Fine grains, dolomite cement, pyrite common, micritic intraclasts: a) texture changes, large grains of quartz, feldspars, and finer matrix: anhydrite, dolomite cement 2. Much coarser grains up to 1 mm.: grains rounded to well rounded, polygonal quartz also present, b. muscovite: anhydrite and dolomite cement: dolomite possibly replacing quartz at some grain boundaries, c. micrite intraclast with square features lying on top of grain 3. Uneven contact between 2. and 3. , still contains coarser grained materials but not as abundant as 2., become less abundant as get farther from 2.-3. boundary: clasts of fine grained anhydrite present: d. particularly dark matrix: e. 4. Coarser grained area similar to 2. - Alot of pelloidal micrite - Laths of anhydrite 262 8tate roster 8812924.5 WW Leagues Breccia- Silty Hicrite dolomite Dolomite, Pelsparite, anhydrite Anhydrite Cement insoluble material quartz pelloids muscovite microcline plagioclase - Intraclasts (commonly polymodal nonplanar dolomite and/or dolomite micrite), mottled, anhydrite cement common throughout thin section - Solution seams with abundant siliciclastics 8tate roster 8812941 Qlassifiieagien Mineralogical Campeeitign Intramicrite and dolomite Micrite Dolomite quartz microcline -trace muscovite -trace pyrite anhydrite 1. Dolomite micrite with infrequent fine siliciclastics generally angular 2. Bimodal quartz; still dolomite micrite but also some coarser nonplanar dolomite: anhydrite cement with large pyrite grains: burrowed 3. Insoluble material, stylolite ? (kind of thick) 4. Bimodal quartz, polymodal nonplanar to planar S dolomite with some anhydrite: intraclastic, burrows at a. 8tate roster rr 4 WWII Laminated Micrite dolomite Dolomite to Siltstone quartz plagioclase anhydrite -trace solution seams biotite 263 l. Equant, unimodal planar S dolomite: size may be controlled by the presence of insoluble material which is between ‘most grains, algal laminations: homogeneous composition, average size 0.1 mm. 2. Dolomite cement, fine grained quartz, feldspars, etc.: average 0.1 mm. Btltc Foster 8312 9 61 . 5 Won Features 8iooosparite Dolomite, dolomite Minor Sand, Anhydrite anhydrite Cement quartz 2 insoluble material 1. Stylolite 2. Dolomite polymodal nonplanar dolomite: dolomitized oolites and ?: anhydrite nodules; large well-rounded quartz: also finer quartz generally with dolomitized "clasts" 3. Replacement dolomite coarser than in 2. also dolomite micrite common somewhat finer siliciclastics 4. Dolomite polymodal nonplanar to planer S coarser than the rest of section, replaces oolites etc., also scattered insoluble material 8tate Poster 88 s a 'ol ,' - - --' . ,-uso i ,-. Laminated Micrite dolomite Dolomite and Siltstone quartz insoluble material anhydrite plagioclase - Laminated . 1. Organics (‘2): finer laminations of this material throughout the thin section , ' . 2. Relatively coarser grain size 0.1 mm.: plagioclase, quartz, anhydrite: area pinches out 264 8tate roster 8812982 . O ' .1 l l- v. 0‘: ._ 'll... o, L. Oosparite Dolomite dolomite with Anhydrite Cement anhydrite 1. Laths of anhydrite 2. Oolite and intraclasts, etc. ghosts; matrix dolomite is generally coarse crystalline nonplanar: infrequent anhydrite 8tate Poster 8812989.2 Classification uinezalegieal gempesition _Eeataree Micrite Dolomite dolomite quartz ~trace - Dolomite micrite with lots of insoluble material and with a trace amount of fine siliciclastics 8tate roster 8812996 Classifiieation ninegalegieal Campoeition Featggee Oosparite Dolomite, Minor Anhydrite Cement - Oolites and other ghosts throughout thin section - Matrix dolomite coarse planar S to nonplanar 1. Solution seams (insoluble material) common note dolomite finer grained in solution seams ' - 265 vuvoaowx nrutwcnonnwowo coop >H oao um: mncooonm. noun comonwvnwo: Eu HHmou no ppmcm an» an. monon monomnoao I maoxovoo ocpoawno oosnoon wanoncooooo ooHoawno oao aconns mmaomnoso no wnoun an” aoumw 99%: siliciclastics 0.04 mm., subangular, < 1% 2. pyrite concentrated here as a boundary between 1 and 3 3. much coarser crystalline material than 1, dolomite rhombs as large as 0.7 mm.: siliciclastics also coarser 0.5 mm., generally rounded: dolomite often as a cement between siliciclastic grains: micrite matrix material also present: 40% siliciclastics, 15% dolomite micrite, 45% dolomite rhombs 4. siliciclastic abundance and size decreased 0.2 mm.: polymodal planar E and planar S dolomite 810018 1-20, 73 glassification flinezalegieal Qomposition Featttee Dolostone dolomite quartz pyrite plagioclase anhydrite - possibly, very minor - homogeneous unimodal nonplanar dolomite, 99% - rounded, 0.1 mm. siliciclastics < 1% 810010 1'20, BA Wu ' Mineralegiealmuien Features Intraclastic Dolostone dolomite ‘ to Silty Micrite quartz Dolomite plagioclase pyrite app! dolo: fract EQEEEL 00108121 271 — lithoclasts - polymodal nonplanar dolomite - siliciclastics 0.1 mm., rounded, more abundant, approximately 15%, in areas between lithoclasts - coarser crystalline dolomite may be neomorphic Riddle 1-20, 91 Qlessifieati2n______nineralesieel_semgeeitien creatures Dolostone dolomite pyrite insoluble residue - polymodal nonplanar dolomite 90%, coarser crystalline dolomite associated with fractures or burrows . - pyrite or insoluble material commonly found in seams or fractures Riddle 1-20, 103 glassification ninetalegieal Qampesition Featatee Dolostone dolomite pyrite - unimodal nonplanar dolomite > 99% - pyrite and siliciclastics < 1% a. anhydrite cement, pyrite Riddle 1-20, 111 Qleeeifieatien______uinerelegieel_£emeesition Eeetures Dolostone dolomite pyrite quartz - Polymodal nonplanar dolomite, > 99%, homogeneous - Pyrite and siliciclastics < 1% the : fract: Seams 272 o o O V l’ : '°. 2 0MP. 0! Micrite Dolomite dolomite quartz ’ orthoclase - Polymodal nonplanar dolomite, 99% - Solution seams in a small area in the upper corner of the section - Pressure solution on a quartz grain - Siliciclastics, 0.25 mm., subrounded to rounded, 1% R1dd1e 1-20, 128 -S . . ° .9 9 l' 0. '° C ° °'_t '! '-. _ s Micrite to Silty dolomite Micrite Dolomite anhydrite pyrite quartz K-feldspar insoluble material - Polymodal nonplanar dolomite, coarser crystalline in fractures - Higher percentage of siliciclastics within solution seams - Burrowed - Pyrite concentrated in solution seams Riddle 1-20, 133 Qlassification ninezalegigal genteeition Featttee Dolostone dolomite quartz plagioclase - Polymodal nonplanar to planar S dolomite, nearly 100% dolomite except where siliciclastics fill in fractures: siliciclastics commonly 0.04 mm., subangular Riddle 1-20, 141 Won W Intraclastic Dolostone dolomite . ' quartz - Siltstone intraclasts, one covering the entire bottom of the section, 8 mm., some intraclasts approximately 0.3 mm. silit silic "dirt silic burro Qis Bimod; [301051 273 - Polymodal nonplanar dolomite - Siliciclastics commonly 0.5 mm., well rounded: siliciclastics 3%, intraclasts 2%, dolomite 95% 8chumachor 1-24, 18 I o o o o - gs. - 0 9 15: Oz -_ 7011-0. 9 '+ - “ Silty Micrite Dolomite dolomite quartz microcline anhydrite -rare chert insoluble material l. Coarser crystalline lamination, 0.2 nmu: siliciclastics rounded - Majority of the thin section is a finer crystalline "dirty" looking ‘material with. grain, size 0.05 mm.: 20% siliciclastics - Coarser crystalline areas may be material filling in burrows 0.15 mm. 2. Siliciclastics as large as 0.9 mm.: dolomite 7% Schumacher 1-24, 28 Qlassifieation Minetalegical Qempeeition Featazes Bimodal Sandy dolomite Dolostone , chert quartz pyrite orthoclase plagioclase microcline - Mixture of finer crystalline "dirty-looking" material. and.a coarser crystalline "cleaner-looking" material: coarser crystalline fraction 0.6 mm. siliciclastics well-rounded: chert abundant: siliclastics 25%, dolomite 75% glee; silty_ Dolom: Sandy. Dolom1 areas DODPIa dOlomi SiZe f dhd dc Eleeeg; I Micri'c 274 8chumachor 1-24, 38 i .1 ll- -_ '1..a oloo_ o! ‘1 Silty Micrite dolomite Dolomite chert quartz pyrite anhydrite -minor microcline - Siltstone "dirty-looking" matrix with some larger dolomite, siliciclastics, chert: coarser size fraction commonly 0.15 mm.: siliciclastics 15%, dolomite and dolomite micrite 85% 8chumachar 1-24, 48 at'on .‘ne . ..' - . --_' . Sandy Micrite dolomite Dolomite quartz orthoclase microcline chert plagioclase pyrite - At both the top and bottom of the section there are areas of nearly pure dolomite this dolomite is polymodal nonplanar dolomte: note at the bottom of the section some dolomite crystals as large as 0.95 mm. - Majority of section: siliciclastics 40%, ranging in size from 0.02 mm. to 0.45 mm., generally rounded: dolomite and dolomite micrite 60% 8chumachor 1-24, 58 :1 'E° !I H' J . J g '!i n F ! Micrite Dolomite dolomite quartz - Polymodal nonplanar dolomite, >99% - Siliciclastics well-rounded, 0.25 mm., 99% - Siliciclastics, rounded, 0.3 mm., <1% 8chumacher 1-24, 88 Wish Jian F u es Dolostone dolomite quartz pyrite insoluble material 1. Dolomite is generally unimodal nonplanar, dolomite has possibly replaced echinoderm fragments, siliciclastics <1%, rounded, 0. 2 mm. , porous areas probably burrows which have not completely filled in 2. As approach top of section see more siliciclastics and solution seams: siliciclastics as large as 0.5 mm. - Note strange pattern at uppermost stylolite Class Dolos Sandy possi round fille. appro; “551.) 001051 276 8chumachor 1-24, 98 ' 0 o o -" 1 '. .2 g 1.71 0‘27 ._ .11..‘ o. ’._ _'- Dolostone to dolomite Sandy Dolostone quartz pyrite insoluble material 1. Dolomite is generally unimodal nonplanar: dolomite has possibly replaced echinoderm fragments: siliciclastics <1%, rounded, 0.2 mm commonly . -porous areas probably burrows which have not completely filled in 2. More siliciclastic-rich and more solution seams as approach top of section: siliciclastics as large as 0.5 mm 8chumachor 1-24, 108 glaeeificatioa ninetalegieal composition .Featttee Dolostone dolomite quartz plagioclase orthoclase - Unimodal nonplanar dolomite - Porous band of siliciclastics crossing section commonly well-rounded, 0.25 mm. ' - Organic material fills a fracture extending down from the above described area: note doesn't contain siliciclastics, only contains dolomite . 8chumachor 1-24, 118 Qaeeifleatim—flnemflieeLeempeeitiQn Features Fossiliferous dolomite Dolostone - Dolomite commonly as a fossil replacement texture - Unimodal nonplanar dolomite as matrix' - Some siliceous material filling in a few fractures 8chumacho§7l-24, 128 -. 5. ° o. 'O 91‘ - 92 ._ ou!~~ 0! Quartz Sandstone quartz dolomite anhydrite chert - Bottom of section polymodal nonplanar dolomite - Majority of section quartz: note area near bottom of section where grains make radiating pattern: coarse grained 8chumachor 1-24, 138 .s O 1. O ‘ 1‘ ;. oo ._ ouo. . a! Interlaminated dolomite Dolostone and Silty quartz Micrite Dolomite plagioclase . chert Ell-l- muscovite -rare q 1. Unimodal nonplanar dolomite 99%: siliciclastics 1%, 0.05 mm. 2. Chert 3. "Dirty", siliciclastics 30%, 0.03 mm. . 4. Siliciclastic-rich: dirty looking matrix: subangular grains, quite variable in size - Coarse chert with anhydrite inclusions 8chumacher 1-24, 148 .ss° 'cat'- .5 - 2 ..f a . --_' 'o e: u -s Intraclastic Silty dolomite Dolostone quartz plagioclase microcline - Intraclasts - Finer matrix, unimodal nonplanar dolomite - Coarser crystalline, polymodal nonplanar to planar S dolomite often associated with siliciclastics, may be filling in burrows , . - Also one area with coarse crystalline planar dolomite cement filling in a fracture 278 8chumachor 1-24, 158 Won Features Fossiliferous dolomite Dolostone siliciclastics - Polymodal nonplanar to planar S dolomite, 99% l. Dolomitized echinoderms - Coarser crystalline dolomite frequently appears to be filling in burrows 2. Solution seams with pyrite 8chumachar 1-24, 168 Qlaeeifieatien Mineralegical tempeeition Featgtes Interlaminated dolomite Dolostone and Silty quartz Micrite Dolomite microcline plagioclase muscovite -' Polymodal nonplanar' dolomite interbedded. 'with siliciclastic rich (90%) laminations: note burrow filled with this material - Organic material present - Siliciclastics are unimodal, note overgrowths on some grains: also polymodal nonplanar to planar S dolomite - Dolomite is also unimodal in laminae that are dominantly dolomite (few siliciclastics), nonplanar 8chumachor 1-24, 178 :1 S 'E' !' H' J . J ; i!' n Interlaminated dolomite Dolostone and Silty quartz Micrite Dolomite plagioclase microcline muscovite pyrite -minor anhydrite -minor chert -trace' 279 1. Mottled (burrowed?) dolomite dominant polymodal nonplanar to planar S: siliciclastics common in areas scattered throughout possibly burrows 2. Siliciclastics more dominant, subrounded, feldspar overgrowths, dolomite as cement 3. Laminated unimodal nonplanar dolomite: infrequent siliciclastics (5%) except in areas where thin to incomplete laminae exist, here dolomite is larger crystalline and sometimes a cement, pyrite common at boundaries of laminae and higher percentage of siliciclastics at 15% 4. Siliciclastic-rich, 85%, unimodal, chert ~trace, subrounded, feldspar overgrowths: polymodal nonplanar dolomite 8chumachor 1-24, 188 :1 'E' !' . H' J . J : ili n Micrite to Silty dolomite Micrite Dolomite pyrite quartz plagioclase microcline insoluble material anhydrite -minor muscovite -trace - Feldspar overgrowths l. Unimodal nonplanar dolomite 2. Dolomite somewhat coarser crystalline that 1. nonplanar: siliciclastics present subangular to subrounded: pyrite at boundaries of irregular laminae 3. Pods of insoluble material with mainly dolomite inclusions and a trace amount of siliciclastics: Surrounding matrix similar to l. 4. Siliciclastic-rich, 60%, dolomite cement, subangular to subrounded 8chumachor 1-24, 198 Cleeeifieatien Mineralseiealimmeitien ' Features Intraclastic Sandy ’ dolomite Micrite Dolomite quartz microcline l. Dolomite micrite laminations , - - 2. Siliciclastics, 15%, subrounded: dolomite becomes 280 coarser crystalline around siliciclastics 3. Siliciclastics, 20%, subrounded, feldspar overgrowths: dolomite micrite intraclasts: dolomite matrix, unimodal nonplanar to planar S 8chumachor 1-24, 208 Classifieetien Mineralegieal_semneeitien Features Sandy Dolostone dolomite ' quartz microcline - Relatively homogeneous: siliciclastics 15 to 20%, subrounded to rounded, dominantly quartz, often strained to polygonal: dolomite matrix unimodal nonplanar to planar-S 8chumachar 1-24, 218 55' 'c 'on Minerelegieel_§empesition Features Intraclastic Sandy dolomite Dolostone quartz microcline insoluble material pyrite plagioclase anhydrite -trace . 1. Polymodal nonplanar to planar-S dolomite: siliciclastics, 30%, subrounded 2. Finer dolomite less siliciclastics than 1. 3. Stylolite (insoluble material and pyrite), fine crystalline nearly pure dolomite above stylolite, various crystal sizes and a ndxture of dolomite and siliciclastics below stylolite 4. Siliciclastics, 30%, subangular to rounded, quartz often strained, often polygonal: dolomite matrix polymodel nonplanar 5. Dolomite micrite intraclasts 281 8chumachor 1-24, 228 0 0 o 9 1‘ a on o. 0110- '1 Sandy Dolostone quartz dolomite microcline chert -rare I anhydrite -minor l. Siliciclastic-rich, 50%, subangular, feldspar overgrowths common: dolomite cement, anhydrite -trace 2. Sandstone with minor dolomite present: siliciclastics may be described like 1. 8chumachor 1-24, 238 .s f,’ . 'o. 1'n-_a_--' a - oos' o. -- uu-s Quartz Sandstone quartz microcline dolomite -trace plagioclase - Siliciclastic-rich, subangular to subrounded: infrequent dolomite: intergranular porosity up to 15% Schumacher 1-24, 248 .ssi_'c- 'on 9' e ._-- .' o .. 't o; Intraclastic quartz Sandstone chert orthoclase insoluble material 1. Intraclasts 2. Silicified oolites - Chert cement 282 8tovona 1-35, 1D ion Features Bimodal Silty dolomite . Micrite Dolomite quartz l 1 microcline chert 2 insoluble material anhydrite l 1. Siliciclastics bimodal, larger grains rounded to well- rounded, smaller grains subangular 2. Chert intraclast with silicified oolites - Mottled appearance due to irregular areas which are dominantly dolomite micrite often with solution seams or siliciclastic-rich with dolomite micrite or cement as matrix - Fine chert scattered throughout thin section, 1-2%: quartz grains often strained, polygonal 8tovons 1-35, 2D is . . :t'l v.1- .. oo .. o oo . o! Bimodal Silty dolomite Micrite Dolomite quartz chert microcline plagioclase dolomite anhydrite -trace - Bimodal siliciclastics in dolomite micrite matrix with some dolomite rhomb's present - Siliciclastics, larger fraction subrounded to rounded, dominantly quartz, often strained some polygonal: finer fraction subangular to subrounded, overgrowths present on some grains Chert relatively common, often as intraclasts, 5% 283 8tovons 1-35, 3D Classifieetien Minerelegieal_£emeesitien Features Quartz Sandstone quartz chert dolomite plagioclase -minor microcline -minor - Quartz-rich, angular to subrounded, often strained some polygonal, infrequently well-rounded with overgrowths - Chert relatively common, note 1. silicified oolite - Fine dolomite scattered throughout planar S to planar E 8tevens 1-35, 4D C 55' ’cat'on Minerelegieel_£emsesitien ezeatures Micrite Dolomite dolomite and Quartz Sandstone pyrite FZJ_ . quartz : L microcline 1. Dolomite micrite, fine pyrite throughout and scattered very fine siliciclastics 2. Coarser dolomite and siliciclastics but dominantly dolomite micrite as in l. 3. Mottled, pods of coarser dolomite also some coarser areas appear to be burrows 4. Coarsening upward, near boundary siliciclastics subangular to subrounded, dolomite matrix: up from boundary dominantly quartz, often with overgrOwths, subangular: fine dolomite rhombs at top possibly another laminae 284 8tovona 1'35, 58 on 9 I‘ ’-_ 01° -. oat-O- °! "'- 7 ': Intraclastic Oolitic dolomite Micrite Dolomite chert ‘ anhydrite insoluble material 1. Large intraclasts within dolomite micrite matrix containing infrequent anhydrite as very fine nodules 2. Mottled dolomite micrite and siltstone material 3. Solution seams 4. Chert and silicified oolites 8tevons 1-35, 6D Qlaesifieatien ninetalegieal Qompeeitien greatntee Interlaminated Micrite dolomite Dolomite and Bimodal quartz 2 Quartz Siltstone microcline ‘ anhydrite chert i ‘ . . 3 muscov1te -rare , ' pyrite 1 4 1. Siliciclastic-rich bimodal , larger grains well-rounded to rounded, finer grains subangular to subrounded, feldspar overgrowths common: dolomite matrix nonplanar to planar E 2. Dolomite unimodal nonplanar, scattered infrequent siliciclastics 3. Dolomite micrite with 15% siliciclastics generally rounded to well-rounded 4. Sandstone, dominantly quartz, overgrowths on rounded grains very common, also microcline and chert, grains generally subrounded to subangular - 285 8tovona 1-35, 7D 0 0 O . O C ’oS- 9 '1 1‘ ._ °' -_ 0110-, 0! "- . ‘r Nodular Micrite dolomite Dolomite chert quartz -trace microcline -trace muscovite -trace , insoluble material 1. Dolomite micrite nodules with solution seams seperating infrequent siliciclastics: note areas of coarser unimodal nonplanar to planar S dolomite , 2. Chert nodules surrounded by dolomite micrite and solution seams 8tevons 1'35, OD WWW Features Micrite Dolomite chert and Oolite dolomite insoluble material muscovite ‘ quartz , plagioclase k 1. Chert nodule within siliciclastic-rich area,. subangular to subrounded, insoluble material 2. Dolomite micrite to polymodal nonplanar dolomite, solution seams relatively common, scattered fine siliciclastics 1% 3. Infrequent chert nodules near contact and possible burrow at a. 4. Silicified oolites 286 8tovons 1-35, 9D Qlaesifieatien Mineralegieal tempeeition Featazee Algal Dolostone dolomite quartz plagioclase muscovite microcline insoluble material 1. Polymodal nonplanar to planar S dolomite: siliciclastics~1% 2. Dolomite very fine, micrite, note brown stylolites within, also coarser crystalline dolomite filling fracture 3. Insoluble material containing siliciclastics with 2% dolomite rhombs 4. Algal laminations, note stylolite then insoluble matrix with mainly siliciclastics 8tevans 1-35, 10D C ass' ' at' iner o ica o os't'on es Interlaminated dolomite Micrite Dolomite quartz and Siltstone plagioclase chart 1 muscovite 2 microcline , insoluble material hornblende‘-rare - Laminated to mottled 1. Siliciclastic-rich, laminated by grain size, insoluble matrix, aubangular, overgrowths common 2. Polymodal nonplanar to planar S dolomite, mottled possibly burrowed, 1 to 2% siliciclastics 287 8tovons 1-35, 11D :1 s 0:. I. II. J a J E 0!. n j ! Laminated Micrite dolomite Dolomite insoluble material quartz muscovite microcline anhydrite - Irregularly laminated - Irregularly laminated dolomite with solution seams or stylolites seperating laminae - Some laminae contain siliciclastics relatively fine grained, subangular - dolomite generally nonplanar* with both polymodal laminae and unimodal laminae 8tovons 1-35, 12D C 55' ° ation Mineralogieal Qompositien Algal Micrite dolomite Dolomite quartz silica cement -minor microcline -trace 1. Algal laminations 2. Polymodal nonplanar to planar S dolomite, some euhedral dolomite rhombs also: mottled, intraclastic 8tevons 1-35, 13D :1 'E' !° H' J . J : ili .F Oolitic Dolostone dolomite chert anhydrite - Oolite-rich dolomite, note some silicified oolites - dolomite generally polymodal nonplanar, dolomite micrite rims on oolites . 288 8tovons 1-35, 148 ss' ' ° ’ ion Dolostone Oolitic chert dolomite insoluble material anhydrite l. Anhydrite nodule 2. Dolomite generally unimodal planar S 3. Stylolite 4. Oolites, silicified, with anhydrite, silica cement, some dolomite 8tovans 1-35, 158 WWI: Features Fossiliferous dolomite Oolitic Dolostone chert - Dolomite is sparry polymodal nonplanar to planar E - Dolomite replaced oolites, fossil fragments, echinoderm fragments, all micritized, algae - Chert present as dolomite replacement texture commonly replacing dolomitized fossils or oolites, silicified 8tovens 1-35, 168 W101: Featmzee Fossiliferous dolomite Dolostone microcline chert anhydrite - Dolomite generally polymodal planar S to planar 8 - Fossil replacement by dolomite, echinoderms - Siliciclastics and anhydrite make up a minor portion of the entire thin section 289 8tovans 1-35, 17D :1 iE' !' n . H' 1 . J : '!° F Interlaminated dolomite Micrite to Silty insoluble material Micrite Dolomite quartz chert -trace microcline - Laminated 1. Siliciclastic-rich, subangular to subrounded, overgrowths common with polymodal nonplanar to planar s dolomite matrix 2. Unimodal nonplanar dolomite with trace siliciclastics 3. Insoluble material Butler 1-12, 18 Qlassifiieation ninetalegieal Qompeeition Featgzee Intraclastic Quartz dolomite Sandstone quartz chert i microcline insoluble material - Siliciclastic-rich, intraclastic - Bimodal siliciclastic-rich, subrounded to rounded, quartz often strained: chert relatively common: microcline overgrowths common 1. Matrix subhedral dolomite and fine siliciclastics 2. Chert cement containing insoluble material, fine siliciclastics and dolomite 290 Butler 1-12, 28 :1 s 'E' l' H' J . l E 'II F l Fossiliferous Micrite quartz Calcite and Quartz calcite Sandstone microcline pyrite 1. Siliciclastic-rich, subrounded to well rounded, bimodal: fossil fragments common: calcite cement: note not grain supported 2. same as 1. but with chert cement instead 3. Fossiliferous with calcite micrite dominant; solution seams Butler 1-12, 38 o o o o o o o S C ,‘l V l- 1..., ; .11... , .2 Micrite Dolomite to dolomite 1r—-——— Silty Dolomite Micrite quartz ‘ I } pyrite r 2 chert ‘ muscovite -rare I 3 microcline r insoluble material % plagioclase 1. Very fine polymodal nonplanar dolomite with pyrite scatterd throughout 2. Distinct contact, siliciclastic-rich at boundary 3. Siliciclastic-rich fine: chert, insoluble material throughout as well as pyrite 4. Fracture filled with coarser siliciclastics, overgrowths common and dolomite present 8ut1012913512, 4a :1 'E' !' ll' 1 .1: ilin Micrite to Sandy chert Micrite Dolomite dolomite quartz pyrite 1. Pyrite nodules 2. Polymodal nonplanar dolomite, appears mottled, possibly coarser dolomite is filling in burrows: 1% siliciclastics 3. Mottled laminae, looks like algal laminae in areas; generally alternating dolomite and dolomite micrite: bimodal siliciclastics appear to be concentrated more in micritic areas, subrounded to rounded: a. chert nodules 4. Dominantly chert, fine dolomite rhombs common Butler 1-12, 58 :1 'E' l' H' J . J ; o .!. n F ! Micrite Dolomite dolomite chert pyrite H t l l - Mottled 1. Burrows filled with coarser crystalline dolomite - In general dolomite is fine polymodal nonplanar 8utlo§ 912012 , 68 Won Features Micrite Dolomite dolomite 1. Polymodal nonplanar dolomite: two intraclasts 2. Solution seams between intraclasts Butler 1-12, 78 :1 'E' !° If 1 i l E III n F ! Interlaminated Silty dolomite Micrite Dolomite and quartz Quartz Sandstone microcline plagioclase anhydrite insoluble material muscovite 1. Siliciclastic-rich laminae, sandstone, feldspar overgrowths BIBLIOGRAPHY BIBLIOGRAPHY Aitken, J. 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