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New Paleozoic frontier play in eastern Great Basin

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:7042172
The discovery of two new oil fields makes the eastern Great basin province one of the most attractive frontier areas in North America. The Grant Canyon field in east-central Nevada produces from Devonian carbonates and has already flowed more than 4 million bbl of oil since its discovery 3 years ago. The Blackburn field discoveries produce from Mississippian siliciclastic and Devonian carbonate sediments in north-central Nevada. These hydrocarbons, as well as the other 12 million bbl of oil produced from eastern Nevada fields, were generated from shallow-water Mississippian siliciclastic sediments that were shed eastward off the Antler Mountains. Some of the hydrocarbons were probably generated during and before the Laramide thrusting event and were consequently trapped in large Laramide thrust structures and folds in eastern Nevada. Some of these structures have since been modified by Tertiary basin-and-range normal faulting, and some hydrocarbons have remigrated into smaller fault traps. Tertiary sediments in these small Tertiary fault traps have been the main target of exploration for the last three decades. This circumstance has precluded a concerted effort to explore Paleozoic sediments in large Laramide-age structures. A new effort is underway to evaluate the potential of Paleozoic sediments in Tertiary fault traps, which may lead to exploration of Paleozoic sediments in large Laramide structures.
Research Organization:
Cedar Strat, Reno, NV
OSTI ID:
7042172
Report Number(s):
CONF-8609129-
Conference Information:
Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 70:8
Country of Publication:
United States
Language:
English