WNW‘HI \ \ 1 NH |H I 4 l \|\ WIH‘IHH. l l l ‘ M TH _ A PROGRAM FOR THE CONSERVAWON OF THE OEL AND GAS RESOURCES Q? ECUADOR, SG'UTH MAERECA Thesis far the Degree of M. S. MECHiGAN STATE COLLEGE View Hugo King “@949 NISTAT THFt-T". I II IUNW R ”HI" LIBIRARI E, ~ ll ml H l l I l 3!“ I'll ll I'M! till I tL—“ 293 00859 3950 This is to C(‘I‘lilll that the tho-sis entitled A Program for the Conservation of the 011 and Gas Resources of Ecuador, South America [rl'csc'utml In] Victor Hugo King has‘ l)t‘€ll m‘vreptvd tmmnls fulfillment nl lllc‘ requirements for Master's “.3 Geology dog“? in M; tit/wok smt Z/M .m/7/7 2 37%; 51-7145 PLACE IN RETURN 80X to remove this checkout from your record. TO AVOID FlNES return on or before date due. DATE DUE DATE DUE nst'rtution MSU Is An Affirmative Action/Equal Opportunity 1 c:\circ\,datoduc pm3p.t A PBOGRAJ‘ FOR THE CONSERVATION 01‘ m: OIL AND GAS RESOURCES Ol' ECUADOR, SOUTH AMERICA By VICTOR HUGO KING A THESIS Submitted to the School of Graduate Studiee of Hidhigan State College of Agriculture end. Applied. Science in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Department of Geology 19% ACKNOWM‘I‘S I wish to express my deep appreciation for the valuable motion: and. aesietance given'by Dr. lilliam A. Kelly of the Geology Department of niohigen State College. who directed thie paper. I am grateful to Dr. Stanard G. Dergquiot. Head of the Department of Geology. Dr. Bonnet 2. Sandefnr and Dr. Jamee I. from of the Geology Department of Hichigan State College, for reading and correcting the original of this paper. I am indebt- : of Quito, Iona- dor, for permitting me to study, during lbbruery 1948. ite re- eomd files and reporte. I wish aleo to acknowledge my debt to Dr. Lee Roy A. Shoemann, Director of Ooneervation Institute of Michigan State College and Er. Percy J. Hoffnaeter. Director of the Department of Conservation and Supervisor of Valle of the State of Michigan, whose help has been invaluable. ii A PROGRAM FOR THE CONSERVATION OF TE OIL AND GAS RESOURCES 01‘ ECUADOR. SOUTH AMERICA ABSTRACT In the paper are outlined the conservation principles which may provide effective and rational utilisation of crude oil and natural as resources of the Republic of Ecuador. South America. Attention is called throughout the paper to the importance of conserving oil, preventing its waste. and to the necessity of a controlled rate of production under a program of conservation. Die conservation measures insure a continuous and adequate simply of petroleum products at a reasonable cost and protect property rights at the same time. lconomic and technical phases are pointed out. Production of petroleum at a rate in excess of market demnd brings physical waste and results in serious disturbance of the industry economr. Excessive capital expenditures. brought about by the drilling of unnecessary wells. lead inevitably to an excessive production rate, and frequently are opposed to efficient producing practices. The technolog of conservation consists in the selection of production methods which will reduce waste of oil to the lowest amount compatible with the interests of the industry. the consum- ing public. and the national welfare. This selection implies a proper understanding of the practical principles of conservation which are based upon a complete knowledge of the nature and be- havior of oil reservoirs, and the manner in which operating con- iii ditions influence the recovery of oil. A major objective of all efficient production practice is to produce oil under the most efficient type of drive. Hence, the oil pools should be managed according to the reservoir energy in order to secure the Optimum recovery. The common types of drive under which oil is produced are: water drive, dissolved- gas drive. gas—cap drive. and gravitational segregation. Ehe recovery obtainable from an oil reservoir depends not only upon the nature of the reservoir. but also upon the manner in which the reservoir is developed and Operated. The factors include well spacing, well completion practice, and use of pressure maintenance and secondary recovery. Authoritative regulation is needed to prevent waste in the oil production. Provisions of modern conservation statutes relating to oil and gas are stated in the paper. !he allocation recommended within pools grants each Operator an equal Opportun- ity to recover the equivalent of the recoverable oil which under- lies his property. preventing drainage across prOperty lines. The allocation among pools should be observed in order that every pool may produce at an efficient rate and have its fair share of the total production allowable. I Tl- 2m SEIKO)! I. II. III. IV. ACUWM ABSTRACT CWTS ILLUSTRATIONS PLATES TABLES IMODWTION Location of the area mnmamm Geologic features a. Coastal plain b. Andean region c. Oriente region Purpose of the study Pram AND NATURAL GAS IN ECUADOR Distribution Geological features of Santa llena Peninsula Oil companies Operating in Ecuador Ecuadorean oil production Types of production PRIHCIPIIIS 03' PDEOLM CONSERVATION A. General Considerations Importance of conserving crude oil . Meaning and objectives of conservation 3. lconemics in Conservation Market demand Control of dominant costs Importance of production rate Need of oil reserves TICHIOIM}! or 3mm PROJECTION A. Oil Reservoirs Introduction Composition and origin of petroleum Accumulation of petroleum Reservoir for petroleum Occurence and distribution of oil iv PAGE ii iv vii viii viii 8338888 SETIOII Types of drive under which oil is produced. a. later drive b. Dissolved-gas drive c. Gas-cap drive 11. Gravitational segregation B. rectors Affecting Recovery Control of factors affecting recovery Date of production Production of water and gas Well completion practice Time of deveIOpment C. Secondary Methods for Increasing Oil Recovery Methods later flooding ‘Gas-repressuring Pressure maintenance Stabilization of crude D. Spacing of Oil and Gas lells Junction of wells Influence of geologic structure and structural position in well spacing [ell spacing in fields under water drive or gas-cap drive Well spacing in fields under dissolvedpgas- drive Effect of plugged send , I. Bumary of Good Practices in htraction of Oil Y. CGSER‘VATIOH STATUTES Administration ‘ Functions of the state regulatory bodies a. Beetriction of flow b. Balancing supply with market demand c. Equitable @portionment 6.. Regulation of oil pool deveIOpnent Unit Operation Provisions of the modern conservation statutes VI. POOL'S ALLOCATION A. Introduction 3. Principles of Allocation Within Pools Definition Principles C. rectors Pertaining to 'aste Prevention Field rules 'ell spacing Control of gas production Control of water production Unifomity of withdrawals PAGE $88 3 8 8&fifififi33B8388338833 assesses $6553 $9888 SECTION Pressure maintenance Regional migration 1). Principles of Allocation Among Pools General considerations Principles Stripper production Restriction to prevent waste Allocation to groups of pools lquitable allocation to each pool VII. CGCLUSIORS VIII. EIOMMDATIONS IX. IBIELIWHY vi PAGE 52 53 53 53 53 53 55 5? 62 Vii ILLUSTRATIONS PAGE FOLLOIIEG Figure l - Position of Ecuador and her Galapagos Islands 1 Figure 2 - Western section of Ecuador. South America 2 Figure 3 - Interpretation of the Andean region in Ecuador according to Wolf (1892) and the sections of the Cordillera Oriental according to TechOpp (1945) 3 Figure 4 - Geological map of the Santa Elena and Colonche districts. southwestern Ecuador 6 Figure 5 - Official map showing the concessions granted by the Ecuadorean Government to the different oil companies 10 Figure 6 - Graph showing production of petroleum in Ecuador. 1925-1946 16 Figure 7 - Eater drive type of oil reservoir 23 Figure 8 - Dissolved gas drive 23 Figure 9 - Gas-cap drive 23 Figure 10 - Gravitational segregation 23 Figure 11 - Foo rapid rate of oil production pulls the water into the bottom of well, and shuts out the oil which is lighter than water 26 Figure 12 - The flow of oil and gas is not restricted in this reservoir 26 Figure 13 - Arrangements of wells providing 10 acre spacing adapted for exploitation of Ecuador Oilfields Ltd... Company. Santa Elena. Ecuador 50 Yiii PLATES PAGE FOLLOWING Plate 1 - A monument erected over a point of the equator line, in San Antonio de Pichincha, 25 kilometers to the north of mito 5 Plate 2 - A cable tool for shallow wells commonly need in Cautivo (La Libertad) 13 Plate 3 - A standard rotary drilling machine used in deep wells in the Tigro field (Santa Elena), Ecuador 18 Plate 4 - The Ecuador Oilfields Ltd" Co. in La Libertad, Ecuador. In the distance can be seen the mating of Santa Elena 14 Plate 5 - rank for crude oil (50,000 bbl.) 1a Libertad Ecuador. Oil tank is without sand fire wall to prevent loss of oil or spread of fire in case of accidental break 14 Plate 6 - A gusher. During the early development period. wells were drilled in without any preparation for control to prevent waste. oil pollution, or fire hazard 49 W Table I - Stratigraphic column of the formations in Santa Elena 8 Table II - Survey of Ecuador Oilfields 13 Table III - Petroleum production in Ecuador, 1946 15 fiction I IRTRODUO TI 0N _§Eo_cation of the area: - The Republic of Ecuador lies between Colombia on the north and Peru on the south and southeast. It occupies the northwestern part of South America (see Fig. 1). The country takes its name from the fact that the equator crosses the country approximately 25 kilometers from Qiito, capi- tal of Ecuador (see Plate 1). Continuing westward into the Pacific. the equator line crosses her island possessions. the Archipelago of Colon. better known as the Galapagos Islands. (1) The country is in the trapics. extending from 1°21 F. lati- tude to 5° 3. Fortunately, nearly half of the area is occupied by the mountains and high plateau of the W; so that it on- Joys a temperate climate. The area of the country, since the protocol of Rio de Jan- eiro of January. 1942. is 267, 844 square kilometers. his cypher includes the 13 Galapagos Islands lying 600 miles west of the Ecuadorean coast. which have an area of 7,844 square kilometers. The population of Ecuador has been estimated at 3,740,871 (Teran, 1943 p. 174). W: - Ecuador comprises three sharply-defined tapographic divisions: (a) the coastal plains or £2535. (b) the Andean region or is . and (c) the Oriente region to the east 1 Name “Galapagos" derived from Spanish word meaning tortoise for which the islands are noted. -1- A T L A N T I C . 0‘33" 0 ca<£:>¢>°. ‘ O O O 0.0 longs -‘ 600 a. I r . t""‘§31:.1.3 ~ .1... ’""""""""" o I l \ \ / I 4 . I ‘\ / sourn \ / ‘\‘__,/ AHSRICA rscxrlc ocean Figure 1.- Position of Ecuador and her Galapagos Islands. of the Andes. The coastal plains is a relatively flat country of tropi- cal aspect. interrupted occasionally by groups of hills and ranges of less than 1700 feet altitude. Many'of these hills are the spurs and outliers of the Andes (see Fig. 2). The Andean region is the mountainous section between the coastal region and the flat Amazon basin of the Oriente region and extends the entire length of the country. It is comprised of three ranges known as the Cordillera Occidental to the west, the Cor- dillera Central in the middle. and the Cordillera Oriental to the east (see Fig. 3). d The two principal ranges of the Andes. the Cordillera Occi- dental and the Cordillera Central. form a double row of peaks about so kilometers apart with a high plateau between, and maintain this form to a surprising extent until its ranges become irregular and diffuse again near the Peruvian frontier to the south. At cer- tain intervals the double row is Joined by a crosswise ridge. or 'knot' which forms connecting links between the Occidental and Central Cordilleras. Between this double row of peaks (2) and ridges connected by knots are the habitable valleys, called 11mg. drained by rivers that cut through one or another of the ranges. These valleys form only about three-eighths of the mountainous 2 Among these peaks is an unequaled group of snowcapped volcanoes. most of them extinct. Some of the more important peaks are the Chimboraso (20,702 feet), the Cotopaxi (19,498 feet), and the Cayembe (19,160 feet). (Grosvenor, 1941). -2... 3.3,”: W _ 3. c“ I; ‘7 J“ g 190 _ £1 0'. g h.. Province 3 I: I '\ A Figure 2.- Western section of Ecuador, South America. (5:33: Kigg I Jung 125g. p.10) region. but they are the habitat of more than three-fourths of the population of Ecuador. The other five-eighths of the Andean Cor- dillera include land over twelve thousand feet in height on which grows only paramo grass. The third cordillera, the Oriental. is less high and con- pact than the others. more irregular. and disconnected from the Cordillera Central. It was discovered in 1945 by the aerial survey of the Shell Ecuador Oil Company (Tschopp, 1945). The Oriente region is divided (Teran. 1948 p. 135) into two sub-regions: one known as the region of the flanks or hdean pla- teaus. which slopes down from the base of the Cordillera Central, at about 4,000 feet altitude to the Cordillera Oriental: the other sub-region is the low, flat Amazon basin which extends to the Peru- vian border, at about 850 feet altitude. The Oriente region is a vast region little known and inhabited by a sparse, partly Indian pepulation. W8 - he geolog of Ecuador has not been worked out in detail except in a few limited areas. At present only most general statements can be made. me broader geologic features of the western part of the country have been fairly de- termined, principally through the works of Rolf (1892 and 1912) and Sheppard (1927. 1937, and 1946). he eastern part of the country has been studied lately by the Shell Company geologists (Tschopp, 1945). a) thal plain: maternary tablasos and Recent marine sediments occur along the western edge of the littoral belt. The -3- in; to lolf (1892) and the sections of the Cordillera Oriental Figaro 5.- Interpretation of the Andean region 'in Ecuador accord- ecoording to Teohopp (1995)- 1 erer u, -m 44.- known Tertiary rocks on the Pacific coastal plains are of Eocene. Oligocene. Miocene, and Pliocene ago. hey are dominantly marine and are chiefly sandstone and shale. In general, Eocene and Oli- gocene rocks make up most of the coastal range. except in the ex— trene‘north of the province of Esmeraldas. where Oligocene and Mio- cene formations are emosed at the surface. b) M: Volcanic rocks of Tertiary and post-Ter- tiary age form almost a continuous mantle over the Andean region. Associated with the volcanics are Cretaceous sediments which may be observed throughout the entire length. Intrusive rocks. which authorities state are pre-Cretaceous in age. consist chiefly of diorites and porphyrites (Rolf. 1892: Miller and Singewald. 1919). It is in these ancient intrusives and associated intruded rocks that nearly all of the mineralisation thus far known occurs. c) W: The Oriente region belongs to the vast geosyncline which extends from the eastern Andes of Venezuela to Argentina. The sedimentary rocks. of this geosyncline in Ecuador. range in age from Triassic to Recent. me Ecuadorean Santiago marine formation of Triassic and Jurassic age has been reported by TechOpp (1945, p. 21) to have characteristics for source rocks of petroleum. And the Rape formation of Cretaceous age has been compared to the Cogollo-Luna-Colon formation in Venezuela and Villeta of Colombia. both productive petroliferous sense. 0 of the : - The purpose of this paper is to present the results of my studies of the petroleum industry of Ecuador. This paper points out principles which may provide .. 4 .. effective utilization of the oil and natural gas resources of Ecua- dor. and recoumnends factors that should be considered in the proper application of these principles. The report is submitted in the hope that it will serve a use- ful purpose in promoting general recognition of these principles and the acceptance of these factors by the regulatory bodies of Ecuador in administering conservation lass pertaining to oil pro— duction. Plate 1.- A monument erected over a point of the equator line, in San Antonio de Pichincha, 25 kilometers to the north of Quito. figction n PETROLEUM AND NATURAL GAS IN ECUADOR W . Though oil and natural gas have been re- ported from the eastern slopes of the Andes in the Oriente region of Ecuador (Sinclair and ”lesson. 1927; TschOpp, 1945) and oil springs in the coastal plain in the provinces of Esmeraldas and Manabi. and in spite of efforts to encourage further emloration in the province of E1 Oro (see Fig. 2), the only region of promise thus far discovered and developed is that of the peninsula of Santa Elena, about 64 miles west of Guayaquil in the Guayas province (see 1'13. 4). The principal oil accumulation occurs. in Santa Elena. in sandstones ranging in age from upper Cretaceous to lower Eocene. The source of this oil is controversial and it is believed that the oil itself is indigenous to the formation in which it now occurs (Thomas. 1946 p. 20). Sheppard (1937. p. 250) assumed that the oil had its origin in the silty shales which make up the greater part of the Tertiary sediments. Seepages of petroleum and productive sands range from the upper Eocene to the Oligocene. and although it is'quite possible that certain shales of the latter formation may have been the cause of the oil in these beds. it is the opinion of Sheppard that the majority of the oil occurrences which are found higher than the Eocene have been occasioned entirely by upward seepage. or migration, along Joint or fault planes. -6- h.» j ' ' .. -;_- . -...l __. - v IVI ' § . 1 ccoLocICAL mar ' “$3.39“? "‘“' SANTA ELENA COLON CHE DISTRICTS * 8.! ECUADOR (0va an 'ODOOMD-u 0' “Ola! “I'DIRO. an s IMILL MD A; I nun-av me Q 1 A 1 1 ‘pmto-fllie . 91 L11 ? 9"“' Uses n~~0 ee-ee'ee' «q It 1 “.‘t \‘¥;\c‘ "Dov saves-ones no - n 9.qu (.1 a” '5. 5],. ;n;"\.\ " nu” one ”.094. l .' \s b ca“ heme "scene‘s-e (3“. “H ~~~‘f. 1.“. >~~~..~e.. ~‘ Jul. . . (-9 "'“H' V 3'“) . A . 'Of .O-w . . “m .. 2:...- . .3: 2, , . .ltli' e‘ “ECO-alt a”... w... ~0- ‘ ._ ' .P' 3 r V ' e‘“ ‘4 t , _ F ‘fl’“‘t~“ ‘w .‘a--,“-.-v- l ‘ i. . . ‘ e . \ e s ‘ ‘ t \ ‘ . 3 . " ‘fi— _ ~_ s~~~~~~-~‘ “Wek _ __ . ; Cement. A-un, _- \ : . l \ ‘ ‘ MGM.” Penn." ' . ~ . ' e (U : _' /4 I V. —-1 "v. +W9‘ \wm‘sz-v-e‘ o 'e e' . ‘ U. 'I “ tends . v \“ .e O ‘5'- | ..3.e.m n . _ Io " \ . . a n3e» v.9... . . leeeiee um “3"»... ~ \ .K ‘ .‘ ‘ ~ efswu‘s‘wwfe 0 e 4 ‘l I - . e — - 4 ~ + . I - "I‘ ‘— "T‘ “I '_"+’ ‘4 - U. u “ u a. m ecologiml .139 of t'te neuron :21 as an; -3101 cie clan-iota, .Soutl.uee'.ern .cuédor. ’Aiter e. e Azrrd 1 j) Geolggical features of Santa Elena Pegnflla: - The Santa Elena region comprises plateaus. known locally as tablazos. and rugged hills generally less than 1.000 feet. Below this surface formation. composed of soft sedimentary rocks of Qaeternary age. a greenish-grey sandstone is found which passes laterally into sandy shales. and in certain localities (Anson) the formation is saturated with a heavy, dark-colored oil. These sandstones and shales are distorted and crushed which makes it almost impossible to map the district satisfactorily. From the viewpoint of petroleum it is important to note that the most saturated oil sends in the Santa Elena region occur in these ex- cessively shattered zones. and are often in close contact with the igneous dyioes intruded into the Tertiary sediments. The thickness of the Tertiary formation is not known. he earth's crust has been broken up into innumerable independent rock blocks. The main blocks are separated from one another by large feailts (Report of the International Ecuadorean Petroleum Company. 1948). These fault-blocks have been tilted in various different directions and have undergone different vertical move- ments. so that some have sunk down while others have been up- heaved. This region has been complicated by igneous intrusions. apparently dykes and sills. that have considerably baked and silicified the adjoining rocks. In general the geology of this area has been very difficult to interpret owing to unconformities. faulting. intrusions. and the lack of diagnostic fossils which have impeded a correct age .. 7 - determination of its geological formations. Geologists of the Ecuador Oilfield Ltd. Company have divided the peninsula into two areas: a) the north area and b) the south- east area (Geological report submitted by the company to the Bur- eau of Mines of Ecuador, 1940). The north area (see rig. 4) has sporadic occurrences of m :3 i? i w;— J dolerite - a volcanic rock - and chert. Ems beds in many places dip very steeply as a result of past tremendous disturbances and crushing forces. The region has a fossiliferous formation. the ‘t’iiln -.- . gab-lame; of Quaternary age. Its thickness varies from 15 to 300 feet. Shallow wells drilled into the buried cherty low masses have found commercial oil accumulation in fissures. The south-east area has sandstones, conglomerates. and clay of Eocene age. In this area are found the I'Seca Shales' and 'So— corro Series” - productive formation in local areas - of the upper locene age. These formations are covered mainly by deposits of Oli- gocene sands and shales. Below the Socorro Series lies the "Clay rabble Bed” and below that the Atlanta formation of shales and. sandstones which is the deeper pay in the important Tigre field area. The "Atlanta Sandstone" of the lower Eocene is over 3,000 feet thick, and wells usually penetrate this for 300 to 400 feet before reaching oil. The stratigraphic formations of the Santa Elena Peninsula are shown in Table I, page 9. Q1 Cmanieg gperatipg in Twp}: - The principal 011 com- panies Operating in Ecuador are: The Anglo—Ecuadorean Oilfields, .. a .. Table I STRATIGRLPHIC COLUMN 0? THE IOBMATIONS IN SANTA mm” Geologic age Eggs gf fgfltiog Thickne gg fit.) @racter ) - 11.1-1‘l" . q< Maa- Li.- Pleistocene Tablasos 80 0 Calcareous deposits 8: gpsun. Hiocene Progreso rm. - - Sandstone 1 (local) ‘ Oligocene Ancon rm. l+00 - Sandstone (local) 4 Oligocene Oligocene Shales - 2850 Clay a shale Eocene Seca Shalee 600 0 Clay with concretions. Eocene Socorro Series 1100 0 Clay as sand- stone (Petrol- iferous eerie). Eocene Clay Pebble Bed 2200 100 Breccias 8. clay Eocene Atlanta Shale 2700 1000 Dark shale d: quartsiferous conglomerate. Eocene Atlanta Sandstone 3570 2500 Hard sandstone a. some clay (Petroliferous eerie . Eocene San Jose Shale N00 1000 Hard. black clay. Eocene San Jose Sandstone - 314-60 Hard sandstone a. some clay (Shows oil traces) (3) Taken from geological reports submitted to the Bureau of mines and Petroleum of Ecuador by the Ecuador Oilfield Ltd. Company and the International Ecuadorean Petroleum Company (Colon 1939. pp. 112. 128) . and the Anglo Ecuadorean Oilfields Ltd. (Piedra 19‘”. p. 81)- .- 9 - Ltd., and The Ecuador Oilfields Ltd. which have a backing of Brit- ish capital. The Shell Company of Ecuador and Esso Standard Oil Company of Ecuador are American-owned concerns. The domestic com- panies are: Gompania Petrolera Ecuatoriana. Carolina Oil Company, Petropolis Oil Company, Concepcion Oil Company, Tompkins Concession, and. lag. Hidalgo Concession (see Fig. 5). Iith the exception of the Shell-Essa companies, which are exploring in the Oriente region, and Compania Petrolera Ecuator- iana. which is exploring in the lowlands of the El Oro province 2 in the southwestern part of the country. the principal activity '1 is confined to the Santa Elena Peninsula in the Guayas province. In 1937. the Shell Company of Ecuador obtained a concession of 33,615,000 acres in the Oriente region of Ecuador. it the end of 1948. the Eeso Standard Oil Company of Ecuador Joined in oil exploration in the eastern region of Ecuador, where Shell has been working for some time. Under the concession Shell and stand- ard were authorized by the Ecuadorean Government to transfer be- tween themselves any of their rights (The Oil and. Gas Journal. vol. 47 n! 29. Nov. 18, 1943). Tremendous difficulties and costly problems associated with thick vegetation have been a serious retarding factor in develop- ing the oil exploration in eastern Ecuador (Showler. 1947). The Shell is carrying on .‘ limited geological and geOphysical survey in this region. Since 1937. four wildca’ts have been completed, two of which reached depths of 5,281 feet (Vuano s2 1) and 7,019 feet (Hacuma 39 1) (Moore 1947 p. 106). no tests were dry. The - 1o - q a“. 9 .04 s \ ‘h—J“ _‘ “afi‘a ‘ zIyIAafi 2. ...j Lope": - 00.000 to D’h is» . all..o‘e(' U IP'I'IJOO 4 ' -‘ru’ 0’4'-0’o.-(- r a “:04 Inpofl - ‘0 l 4!! U. .17 1r“. In“. in. R ‘E L Jc‘o ~50M'0110‘v-ue . ”001000 V) 6‘ . m f a ‘0 0_e_0_-_ 10/ ‘Zfib'f-‘VM.’I/.’/7fl7ffl ..-._. _' ’ "— ."‘-0 (m7 ‘I’"I'-); at “'vrra y pt ": In: a, / .11 0514.0 r‘-r’dll / DO. “I s’ / ,4) p 1 . . “' : A: - Figure 5.- Official flap showing :Le concessions Lrnnt d Ly tic Ecuadorean Lovernnent to the different oil comfanico (After {iedra, 124z u. 1%) actual exploration for oil in this region is extremely difficult and results may be slow in materializing. but the outlook for possible large production is more favorable than in the already producing region of Santa Elena. If and when production comes about. it will be accompanied by improved transportation facili- ties that will Open the way for general economic development of the region. During 1947, the International Petroleum Company completed its extensive search for oil in the coastal regions of Ecuador in the provinces of Gnayas. flanabi and Esmeraldas. In ten years of exploration the company drilled 20 wildcats. two of which reached depths of 13,205 feet (Badada :2 1). which is the deepest well drilled in South America, and 10,485 feet (Rodeo s9- 2) located in the hauls-Guayas concession of the Guayas province (Piedra. 1947 p. 104). All tests were dry. The Anglo-Ecuadorean is Ecuador's largest oil producer. From 1935 to the present, shallow and deep drilling and deveIOp- ment of the important Atlanta Sandstone formation at about 4,200 feet, have lsspt Anglo-Ecuadorean's yearly production at about 2,000,000 barrels. This company has a refinery, built in the north side of the peninsula at La Libertad. with a daily capacity of 2.700 barrels. The Ecuador Oilfields Ltd. is the second largest producer of the country. This company discovered the important field. El Tigre. situated near the town of Santa Elena. Part of the Atlanta sand oil sons in its Tigre field has been developed into produc- -11.. tion at the rate of 1.400 barrels per day. The company has a small refinery at Cemtivo. near La Libertad, with a daily capacity of 500 barrels. The company manufactures gasoline, naptha. kerosene, diesel oil and residual fuel. The domestic companies are unimportant because of their in- significant production. Emg g1 Production: - Petroleum in Ecuador is locally important and of unusual interest because the oil seepages of the Santa Elena peninsula seem to be the locality of the first dis— covery of petroleum in South America. The petroleum workings are of great antiquity. There is evidence for the belief that they were known to the Indians and later Operated by the early Span- iards about 1500. In 1700 oil was reported fras dng pits at Santa Elena (Eager. 1939 p. 30). In 1917-1922 the annual output ranged from 50,000 to 60,000 barrels, all derived from shallow pits. In 1923. a 45-barrel well was completed and the annual production rose to 87,000 barrels. At that time numerous hand-dug pits were made in San Lorenzo (in the Santa Elena region), the pits being grouped closely together. and the majority of these started in the Quaternary surface rocks. The pits were excavated to a depth of 15 to 50 feet. At the time when the pits of this area were in full operation (1926) the annual output was 350,000 barrels. The low costs of labor and production. and the steady narlset made this business very profitable in those days. However, after heavy rains in the years 1925-1926, these pits were completely flooded and the maderity were mined and abandoned. In 1928, deeper drilling, - 12 - >WF 11?». “.K usually to 1500-2500 feet. showed other producing areas and zones and the output was 1,000,000 barrels. In 1937. it was 2,000,000 barrels. (Thomas. 1946 p. 26). enrlng 1945. a soc-barrel well was completed. at 4200 feet in the northern part of El Tigre field. or Ecuador's total production in 1946 (about 2,322,603 barrels) a single coupany, the Angloquadorean. accounted for almost 75% of the total production. The company's annual production in 1946 was reported to be 1,673,915 barrels. Of this company's production, about 1,240,779 barrels were exported to Argentina and Uruguay, and. the rest was refined and marketed in Ecuador (see Tables II and III). Ecuador's cumulative production at the end of 1947, all from the Semta Elena peninsula. has been reported (Weeks, 1948 p. 1093) to be about 41,800,000 barrels. The annual production in the same year was 2,281,000 barrels (Egloff, 1948 p. 263). of odnotionx - Shallow production to depths of laoo'rect. and of relatively minor importance. is obtained by digging by hand or by drilling with cable tools at 'El Tambo, Gmtivo. Carolina, and Santa Rita fields in the peninsula. The shallow production is obtained from Quaternary to upper Eocene beds (Socorro Series). (see n... 2). The deeper production, to depths of 5000 feet. is the more important and is drilled with hydraulic-rotary system at Con- cepcion, Anson, and Tigre fields. nose wells are producing from theAtlanta Sandstone formation of lower Eocene age (see Plate 3). The oil which is produced from both the shallow and from -13.. 1mm“ 5 -4 Plate 2.- A cable tool for shallow wells Commonly used in Cautivo (Le Liberted). Plate 5.- A standard rotary drilling machine used in deep wells in the Tigre field (Santa Elena), Ecuador. flame of field. glowing M Table L; SURVEY or ECUADOR on. FIELDS (1“) roduci wells well; do the ft Ancon 39 hlh 1200-3800 "Cautivo 28 500-1200 Carolina 15 30-600 Concepcion 10 3000-14000 El Tambo 6 1200 Santa Rita 3’4 500-1200 Tigre L0 1 2350-1550 W 1&9 512 lemm%::§o 92%,, ‘ pflaosggsgg 35,000,000 m. Production bbl “750 30 95 30 10 165 320 6000 Ancon Tigre Total £13, A.P.I. 36-h]. 35 13—23 38 39 23 39 (14) Taken from The 011 and. Gas Journal. Doc. 28 19%. Vol. 148. p- 191. -14.. [1117'- w.