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    Petroleum SystemsPetroleum Systems(Part One)(Part One)

    Source, Generation, and MigrationSource, Generation, and Migration

    GEOL 4233 ClassGEOL 4233 ClassJanuary 2008January 2008

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    Petroleum Systems

    Source RockSource Rock

    Migration RouteMigration Route

    Reservoir RockReservoir Rock

    Seal RockSeal Rock

    TrapTrap

    ElementsElements

    GenerationGeneration

    MigrationMigration

    AccumulationAccumulation

    PreservationPreservation

    ProcessesProcesses

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    Petroleum System Summary

    Source (Material and Rocks)

    Generation (Maturation)

    Migration

    Trap

    Reservoir

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    Source Material

    Non-Biogenic Origins

    Biogenic (Kerogen) Host rock (Shales and Coals)

    Kerogen Types

    Type I Algal (oil prone) sapropelic

    Type II Mixed

    Type III Woody (gas prone) humic

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    Siljan Ring

    Inorganic Gas Prospect

    Drilled to ~22,000 in 1987

    Found abiogenic methane,

    but no poro-perm

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    Sedimentary Rocks Where the Action Is

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    Source Material

    Non-Biogenic Origins

    Biogenic (Kerogen Types)

    Type I Algal (oil prone) sapropelic

    Type II Mixed

    Type III Woody (gas prone) humic

    Host rock (Shales and Coals)

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    Types of PetroleumTypes of Petroleum

    Oil and gas are formed by the thermal cracking ofOil and gas are formed by the thermal cracking oforganic compounds buried in fineorganic compounds buried in fine--grained rocks.grained rocks.

    Algae = Hydrogen rich = OilAlgae = Hydrogen rich = Oil--proneprone

    Wood = Hydrogen poor = GasWood = Hydrogen poor = Gas

    --proneprone

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    Kerogen TypesKerogen TypesType 1 Type 2 Type 3

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    From the Paleontological Research Institute

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    Ganges Deltaic

    Sediments

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    Modern Mahakam Delta Plain

    East Kalimantan, Indonesia(A Rich Source of Kerogen)

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    Inferred Middle Booch Depositional Environments

    Arkoma Basin in Oklahoma

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    Source Material

    Non-Biogenic Origins

    Biogenic (Kerogen Types)

    Type I Algal (oil prone) sapropelic

    Type II MixedType III Woody (gas prone) humic

    Host Rock (Shales and Coals)

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    The Origin of PetroleumThe Origin of Petroleum

    OrganicOrganic--richrichSource RockSource Rock

    Thermally MaturedThermally MaturedOrganic MatterOrganic Matter OilOil

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    Source Rock for PetroleumSource Rock for Petroleum

    Organic-Rich Thin Laminae

    3.39 378

    TotalOrganicCarbon

    LOMPOC Quarry Sample

    Monterey Formation, CA

    HydrogenIndex

    1 Inch1 Inch

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    Woodford Shale (Oklahoma)

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    Channel-Fill Sandstone Resting on Marine Shale

    Red Fork (Oklahoma)

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    Coals and Coaly Shales

    San Juan Basin (New Mexico)

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    Source rock kerogen can

    be correlated to oil/gasfound in carrier beds

    and reservoirs

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    T.O.C.

    Total Organic Carbon

    Basinal Summary Chart

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    Petroleum System Summary

    Source (Material and Rocks)

    Generation (Maturation)

    Migration

    Trap

    Reservoir

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    The Petroleum KitchenTemperature-Pressure-Time

    Geothermal Gradient: (thermogenic hydrocarbons)

    Range:

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    Hydrocarbon Occurrence & Thermal Maturity

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    Oklahoma

    Geologic Provinces

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    Map of Oklahoma Oil and Gas Fields; Distinguished By GOR and Coalbed Methane Production. From Boyd (2002)

    (GOR Cutoffs: Oil 20,000)

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    Schematic Cross-section of the Anadarko BasinModified from Witt and others (1971).

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    Regional Stratigraphic Cross-Section(Hung from Top of Booch)

    Oklahoma Arkoma Basin (Booch)

    (Present burial depth not necessarily maximum burial depth)

    DIVISIONS OF GEOLOGIC TIME Age (approx.)in millions of

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    Geologic Time ScaleModified From Harland (1990) and Hansen (1991).

    Eon Era Period Epochin millions of

    years

    Cenozoic

    Mesozoic

    Paleozoic

    Phanerozoic

    Carboniferous

    Pennsylvanian

    Mississippian

    Tertiary

    Quaternary

    Cretaceous

    Jurassic

    Triassic

    Permian

    Devonian

    Silurian

    Ordovician

    Cambrian

    Holocene

    Pleistocene

    Pliocene

    MioceneOligocene

    Eocene

    Paleocene

    Late

    Early

    Late

    MiddleEarly

    Late

    Middle

    Early

    Late

    Early

    Late

    Middle

    Early

    Late

    Early

    Late

    Middle

    Early

    Late

    Early

    Late

    Middle

    Early

    Late

    Middle

    Early

    0.010

    1.6

    5

    23

    35

    57

    65

    97

    146

    157

    178

    208

    235

    241

    245

    256

    290

    303311

    323

    345

    363

    377

    386

    409424

    439

    464

    476

    510

    517

    536

    570

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    Arkoma Basin

    Estimated Overburden Removal

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    Petroleum System Summary

    Source (Material and Rocks)

    Generation (Maturation)

    Migration (Expulsion)

    Trap

    Reservoir

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    Source Rock for PetroleumSource Rock for Petroleum

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    Source Rock for PetroleumSource Rock for Petroleum

    Organic-Rich

    Thin Laminae

    LOMPOC Quarry SampleMonterey Formation, CA

    1 Inch1 Inch

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    Migration Pathways

    Hydrocarbon Expulsion

    Vertical vs. Horizontal Migration

    Residual Saturations

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    Base

    men

    t

    GEOGRAPHIC EXTENT OF PETROLEUM SYSTEM

    Present-Day

    STRATIGRAPHIC

    EXTENT OF

    PETROLEUM SYSTEM

    Petroleum accumulation

    Top of oil window

    Bottom of oil window

    Trap TrapTrap

    Seal

    Reservoir

    Source

    Underburden

    Overburden

    A A

    Magoon and Dow, 1994Magoon and Dow, 1994

    PresentPresent--Day Petroleum SystemDay Petroleum System

    Inferred Middle Booch Depositional Environments

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    Inferred Middle Booch Depositional Environments

    Arkoma Basin in Oklahoma

    Petroleum SystemPetroleum System

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    Spill PointSpill Point

    Seal Rock(Mudstone)Reservoir Rock

    (Sandstone)Migration fromKitchen

    1) Early Generation

    2) Late Generation

    Gas displaces all

    oil

    Gas beginning todisplace oil

    Displaced oil

    accumulates

    Petroleum Systemy

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    The Leaky Trap

    Petroleum System ProcessesPetroleum System Processes

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    Petroleum System ProcessesPetroleum System Processes

    120 F120 F

    350 F350 FGenerationGeneration

    MigrationMigration

    Seal RockSeal Rock

    ReservoirRockReservoirRock

    OilOil

    WaterWater

    GasCapGasCap

    EntrapmentEntrapmentAccumulationAccumulation

    SourceSourceRockRock

    Schematic Migrational Pathways

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    g y

    From Basin to Shelf

    Asphalt Seep

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    Viola Limestone (Oklahoma)

    The End of the Road

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    On to the Trap

    One More Thing.

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    Basin Assignments

    North American San Juan East Texas

    Gulf Coast

    Anadarko

    Arkoma

    Powder River

    Wind River

    Green River

    Williston

    Delaware

    Midland

    Black Warrior

    Fort Worth

    Others..

    F t t C id

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    Facts to Consider

    Basin

    Location, Size, Maximum Depth, Age (from basement to outcrop + max subsidence), Stratigraphy

    Other items; eg - Structure (extensional, compressional)

    Petroleum SystemSource Rocks: Name(s), kerogen type(s), TOC, depth to top of oil window, kitchen location

    Migration Pathways: Carrier bed(s), faults, distance (vertical and horizontal)

    Traps: Structural, Stratigraphic, Combination (dominant type)

    Reservoirs: Names, Rock types (both reservoir and seal)

    Representative Fields (The biggest ones)

    OOIP, OGIP, RF, Cum Prod

    Other notable Facts anything else you want to add (history, technology, companies, etc)

    Powerpoint presentation: 10-12 slides (or more), approach as management presentation in which object is to highgrade

    future exploration opportunities for your company. For any answers you cannot find, treat as source of increased risk of entry.

    Map of Selected Sedimentary Basins

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    1-Williston Basin

    2-Powder River Basin

    3-Denver Basin

    4-Salina Basin

    5-Forest City Basin6-Kennedy Basin

    7-Big Horn Basin

    8-Wind River Basin

    9-Laramide Basin

    10-Washakie-Red Desert B.

    11-Green River Basin

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