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Petroleum Geology Class 745
Petroleum Generation Petroleum Geology Class 745 Spring 2002 Istvan Csato University of South Carolina Department of Geological Sciences
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I. Organic Matter II. Petroleum Generation III. Source Rock Evaluation
IV. Thermal Maturation Models
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Sequence Stratigraphy
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Controls on total organic matter
Productivity Grain size Sedimentation rate Oxidation/Reduction
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Preservation of Organic Matter
Demaison and Moore, 1980
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Conversion of Organic Matter
biopolymers bitumen biomarkers Barker, 1996
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II. Petroleum Generation
I. Organic Matter II. Petroleum Generation III. Source Rock Evaluation IV. Thermal Maturation Models
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Conversion of Kerogen Organic matter: 1% Kerogen 90% Bitumen 10%
Barker, 1996
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Kerogen Evolution Paths
Tissot et al., 1974
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Variation of the HC/TOC, Los Angeles and Ventura Basins
Philippi, 1965
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Depths and Temperatures for Onset of Oil Generation
Tissot et al., 1975
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General Scheme for Hydrocarbon Formation
Tissot et al., 1974
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III. Source Rock Evaluation
I. Organic Matter II. Petroleum Generation III. Source Rock Evaluation IV. Thermal Maturation Models
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Questions for exploration geologist:
Does the the rock have sufficient organic matter? Is the organic matter capable of generating? Has this organic matter generated petroleum? Has the generated petroleum migrated out? Is the rock oil-prone or gas-prone?
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Quantity of Organic Matter:
TOC must be greater than 0.5% Type of Organic Matter:
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Thermal Alteration Index, Paris Basin
Maturity Thermal Alteration Index, Paris Basin Correia, 1971
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Kerogen Maturation Profile, Louisiana Gulf Coast
Maturity Kerogen Maturation Profile, Louisiana Gulf Coast Vitrinite: woody, Type III kerogen Barker, 1996
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Vitrinite Reflectance Data
Maturity Vitrinite Reflectance Data Dow and O’Connor, 1982
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Vitrinite Reflectance Profile, Elmsworth Field, Canada
Maturity Vitrinite Reflectance Profile, Elmsworth Field, Canada Welte et al., 1984
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Disturbing of Vitrinite Reflectance
Barker, 1996
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Elemental Data For Kerogen
Peters, 1986
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Pyrolysis Increase of S1 with Depth S2 S1 Tmax Barker, 1996
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Pyrolysis Yield of Hydrocarbons with Increasing Temperature Tmax S2 S1
S2/TOC = HI S3/TOC = OI S1 S2 Tmax Barker, 1974
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Changes in TR and Tmax Espitalie et al., 1977
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HI versus OI Peters, 1986
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Evaluation of Geochemical Parameters
Peters, 1986
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IV. Thermal Maturation Models
I. Organic Matter II. Petroleum Generation III. Source Rock Evaluation IV. Thermal Maturation Models
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Kinetics of Chemical Reactions
KER = BIT + RESIDUE At t=0 KER= Vo, BIT=0 At t>0 KER=Vo-Vt, BIT=Vt dV/dt= k(Vo-Vt) k=A*e[-E/RT] Arrhenius equation R =Gas constant ( KJ/mol0K) T=absolute temperature E=activation energy A=frequency factor
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Activation Energy Barker, 1996
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Bond Energies March, 1985
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Increasing Reaction Rate with Temperature
Barker, 1996
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Bitumen Release Curves with Different Activation Energies
Barker, 1996
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Bitumen Release Curves with Different Frequency Factors
Barker, 1996
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Increase in Reaction Rate
Barker, 1996
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Bitumen Release Curves for 8 Parallel Reactions
Juntgen and Klein, 1975
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Distribution of Activation Energies, Paris Basin
Tissot et al., 1987
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Temperature Factors used by Lopatin
Dmaturity = (Dti)(rni) TTI (Time-Temperature Index) Barker, 1996
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Burial History Plot Barker, 1996
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Calculated TTI Barker, 1996
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Calibration of TTI Waples, 1980
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Time-Temperature Reconstruction, Big Horn Basin, Montana
Hagen and Surdam, 1984
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Kinetic Model of Tissot and Espitalie, 1975
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Kinetic Model of Sweeney et al., 1987
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