Petroleum System Modeling in the Interior Salt Basins, North Central ...

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Conclusions ‣ Upper Jurassic Smackover lime mudstone beds served as an effective regional petroleum source rock ‣ Initiation of the generation of hydrocarbon from Smackover in the Early to Late Cretaceous and continuing into the Cenozoic ‣ Peak oil expulsion occurred in the mid Early to Late Cretaceous, and peak gas expulsion in Early-Mid Tertiary.
Page 1 and 2:
Petroleum System Modeling in the In
Page 3: Introduction
Page 6 and 7: Methodology of Basin Model
Page 8 and 9: Absolute Age - Geologic time scale:
Page 10 and 11: Structure Map Top of UK in MISB Top
Page 12 and 13: Isopach Map LK - UK Cotton Valley -
Page 14 and 15: Lithology 45% LST 50%SHL 5% SST End
Page 16 and 17: 0 porosity 0.00 0.10 0.20 0.30 0.40
Page 18 and 19: Methodology: Thermal History ‣ He
Page 20 and 21: Potential Source Rocks Visual Forma
Page 22 and 23: Burial, Thermal Maturation, Hydroca
Page 24 and 25: North Louisiana Salt Basin Cross Se
Page 26 and 27: Source Rock Thermal Maturity
Page 28 and 29: Thermal Maturation History Profile
Page 30 and 31: Monroe Uplift Cross section Locatio
Page 32 and 33: Thermal Maturation Profile Cross Se
Page 34 and 35: Thermal History Profile Monroe Upli
Page 36 and 37: Mississippi Interior Salt Basin
Page 38 and 39: Mississippi Interior Salt Basin Cro
Page 40 and 41: Source Rock Thermal Maturity
Page 42 and 43: Thermal Maturation History Profile
Page 44 and 45: Event Chart for Smackover Petroleum
Page 46 and 47: Manila Sub-Basin Cross Section
Page 48 and 49: Thermal Maturation Profile Cross Se
Page 50 and 51: Burial History Profile Manila and C
Page 52 and 53: Hydrocarbon Expulsion Plot Manila a
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Petroleum System Modeling in the Interior Salt Basins, North Central ...

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