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Previous HitOILNext Hit TYPES OF THE ALASKAN NORTH SLOPE—A PROGRESS REPORT

LILLIS, Paul G., U.S. Geol Survey, Denver Federal Center, Box 25046, Lakewood, CO 80225, [email protected], PETERS, Kenneth E., U.S. Geological Survey, 345 Middlefield Road, MS 969, Menlo Park, CA 94025, and MAGOON, Leslie B., U.S. Geological Survey, 345 Middlefield Road, MS 969, Menlo Park, CA 94025

Previous HitOilNext Hit typing on the North Slope of Alaska has been a challenge for geochemists for more than 25 years because many of the Previous HitoilNext Hit accumulations are mixtures of Previous HitoilNext Hit types, and for some of the source formations, more than one Previous HitoilNext Hit type has been generated because of organic facies variation. A further complication is that crude Previous HitoilNext Hit composition is influenced by non-genetic effects, such as thermal maturity of the source rock at the time of expulsion, and biodegradation and cracking of the Previous HitoilNext Hit after expulsion. Significant progress has been made in recent years with a growing number of Previous HitoilNext Hit samples - using newer analytical techniques and chemometric analysis.

This study reviews the geological and geochemical interpretations from previous North Slope studies and presents recently acquired geochemical data to better identify and distinguish end-member and mixed Previous HitoilNext Hit types. At least ten end-member Previous HitoilNext Hit types have been identified. Probable source formations for the Previous HitoilNext Hit types include the Carboniferous-Permian Lisburne Group (includes the Kuna Formation), Triassic Shublik Formation, Triassic-Jurassic Otuk Formation, Jurassic-Cretaceous Kingak Shale, Cretaceous Torok Formation, pebble shale unit, and Hue Shale (includes the gamma ray zone or GRZ), and the Tertiary Canning Formation. Recognition and mapping of Previous HitoilNext Hit types provide the basis for defining and mapping petroleum systems that incorporate the geologic framework, source rock distribution, burial Previous HithistoryNext Hit, and migration pathways.