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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
Abstract
AAPG Bulletin, V.
2004. The American Association of Petroleum Geologists. All rights reserved.
General Levalle basin, Argentina: A frontier Lower Cretaceous rift basin
Robert E. Webster,1 Gualter A. Chebli,2 J. Fritz Fischer3
1Hunt Oil Company, 1445 Ross at Field, Dallas, Texas, 75202; [email protected]
2Phoenix Oil 
Gas S. A., Lavalle 710, 3
, Of. D, 1047 Buenos Aires, Argentina; Instituto de Gas y del Petr
leo, Facultad de Ingenier
a (UBA), Las Heras 2214, 3. 1127 Buenos Aires, Argentina; [email protected]
3Fischer Petrologic, 16858 West 73rd Place, Arvada, Colorado, 80007; [email protected]
AUTHORS
Robert Webster has a B.S. degree in geology from the University of Colorado (1967) and an M.S. degree from the University of Texas at Arlington (1978). After 16 years of both international and domestic work, Webster joined Hunt Oil Company in 1988 as a senior geologist in international exploration. He has initiated or evaluated frontier exploration plays in virtually every country in Latin America, as well as parts of Africa and the Middle East, and was Hunt's general manager in Argentina in 1993
1994. Webster is past president of the Dallas Geological Society (DGS) and the DGS International Group.
Gualter Chebli obtained a master's degree in geologic sciences (1966) and petroleum engineering (1968), and a Ph.D. in geologic sciences (1973) from the University of Buenos Aires. After a career with YPF from 1968 to 1991 as geologist and ultimately exploration contracts manager, he founded the consulting firm Phoenix Oil Gas S.A. He is professor at the University of Buenos Aires and others, and he is current president of the Asociacin Argentina de Gelogos y Geofsicos Petroleros.
Fritz Fischer has a B.A. degree and a Ph.D. from the University of California, Santa Barbara. He has taught at the University of Nevada, Reno, the University of California, Santa Barbara, and the University of Texas at Arlington. Since his academic career, he has worked in minerals exploration, consulting petrology and, most recently, well-site geology in Argentina, Portugal, and Madagascar.
ACKNOWLEDGMENTS
We thank Hunt Oil Company for permission to present this paper, which represents the culmination of work by many individuals within the company. Carlos Urien provided initial insight and regional interpretation. Dick Boyce and Bruce Hinton did initial and final geophysical interpretations, respectively. We appreciate the constructive comments of AAPG reviewers Wallace Dow, Brian Horn, and Ernest Mancini, as well as Editor John Lorenz, which helped to improve the quality of the paper.
ABSTRACT
The General Levalle basin forms a long, narrow, and deep Early Cretaceous intracratonic rift in southern Crdoba province, Argentina. It trends approximately north-south for more than 150 km (93 mi), ranges from 5 to 50 km (3 to 31 mi) wide, and is more than 6500 m (21,325 ft) deep. Below a prominent middle Cretaceous unconformity, steeply dipping normal faults bound tilted graben and half-graben fault blocks. The lower rift-fill section, the General Levalle Formation (new formation name), is a ValanginianHauterivian siliciclastic and evaporite package more than 3200 m (10,500 ft) thick. It was deposited in an arid, restricted, rift basin that included a hydrologically closed saline lake. Nine lithology-based members represent one continuous cycle of deposition, with a lower coarse clastic sequence gradually fining upward into an evaporite member and then coarsening upward again to an upper sandstone. The uppermost rift-fill sequence, the Guardia Vieja Basalt (new formation name), is a series of Aptian basalt flows and sills more than 800 m (2625 ft) thick, with some thin red-bed intervals. Unstructured Upper Cretaceous to Pleistocene strata overlie the buried rift basin.
Following an extensive exploration campaign, in 19951996 the first exploratory well in the basin tested a deep-seated anticline to 5179 m (16,991 ft), but encountered just one minor show. Reservoir-quality sandstone occurred only in the upper rift sandstone member, but this lacked adequate seals. Deeper sandstone beds were tightly cemented, and basin-center dark shale below the evaporite member was thin, surprisingly low in total organic carbon, and overmature for oil. Although additional geological, geophysical, and geochemical work could have improved predrill understanding and risk evaluation, in the end, only drilling the wildcat determined the actual subsurface situation. It is now evident that given the narrow, deep depocenter, unfavorable reservoir-seal relationships, and a paucity of source facies, an effective petroleum system probably never existed in the basin.
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