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Title: The hydrocarbon potential of the Ene Basin (Peru)

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:6107124

The Ene basin is located between 10[degrees]30' and 12[degrees] latitude south in the foothills of the Eastern Cordillera. Geochemical analysis indicate the presence of mature organic-rich source rocks in the Upper Paleozoic. In particular the Ene formation includes mature (Ro = 0.7 to 0.9%) oil-prone shale with mixed type I/II kerogen. Geohistory models show that the Ene formation entered into the oil window some 5 to 3 m.y. ago in the deep part of the basin and could generate hydrocarbons until the present time. Good reservoir sandstones (Oriente gr., Vivian Fm.) were deposited during the Cretaceous sandstones. The Ene basin extends in a northwest-southeast direction between the Eastern Cordillera to the west and the Shiro-Vilcabamba uplift to the east. The Late Miocene-Pliocene Quechua phase III deformed the sedimentary series producing east verging imbricated thrust sheets and large anticlines which could trap the hydrocarbons generated by the Upper Paleozoic source rocks. Several anticlines are still sealed by the Tertiary cover and represent attractive prospects for hydrocarbon exploration. With a prospective area close to 8000 km[sup 2] the unexplored Ene basin is awaiting imaginative geologists and geophysicists to demonstrate its potential.

OSTI ID:
6107124
Report Number(s):
CONF-930306-; CODEN: AABUD2
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (United States), Vol. 77:2; Conference: International congress of the American Association of Petroleum Geologists (AAPG), Caracas (Venezuela), 14-17 Mar 1993; ISSN 0149-1423
Country of Publication:
United States
Language:
English