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Title: Petroleum systems of the Burgua Depression, Tachira and Apure states, Venezuelan Andes

Journal Article · · AAPG Bulletin
OSTI ID:421160
;  [1];  [2]
  1. E.I.G. Litos C.A., Caracas (Venezuela)
  2. Corpoven S.A., Puerto La Cruz (Venezuela); and others

The Burgua Depression (southeast extension of the Tachira Depression) underwent a severe subsidence during the Andean orogeny. Its tectonosedimentary evolution was controlled by Paleozoic discontinuities. The sedimentary sequence contains Jurassic/Lower Cretaceous syn-rifting transgressive rocks, synDeformational Paleocene/Eocene and Neogene rocks. Deformation is diachronic from SE (Oligocene) to NW (Pleistocene). From oil-rock correlation data, Navay and Los Cuervos samples render excellent potential source rocks. The analyses indicate a marine algal-bacterial organic matter source for Navay and higher plants for Los Cuervos, which plot as moderate yield type II kerogen and low yield type II-III, respectively. Although, the samples are immature (0.50-0.55% R6), ID modelling (BasinMod) suggests that they reached maturation during the Andean orogeny. Oil seeps correlate with Navay and Los Cuervos and were expelled at the peak of oil generation (0.85-0.90% R{sub o}). These source rocks define the Navay-K/T(!) and Los Cuervos-K/T(!) petroleum systems. Potential clastic and carbonatic reservoirs were identified in surface and wells. The Guafita Formation is the regional seal, never extending northward of the Brujas High. Modelling indicates that migration started during late Pliocene and took place northward and south/southeastward of the Andean foredeep.

OSTI ID:
421160
Report Number(s):
CONF-9609255-; ISSN 0149-1423; TRN: 96:005770-0145
Journal Information:
AAPG Bulletin, Vol. 80, Issue 8; Conference: American Association of Petroleum Geologists (AAPG) international conferences and exhibition, Caracas (Venezuela), 8-11 Sep 1996; Other Information: PBD: Aug 1996
Country of Publication:
United States
Language:
English

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