introduction to oil and gas

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    INTRODUCTION TO OIL & GAS

    Dr Deva Ghosh

    Professor in Geophysics

    Head Center of seismic Imaging ( C.S. I )

    30/11/2011

    UTP Course

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    World Energy Sources

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    Future Prospects of Oil & Gas

    Oil

    Gas

    Coal

    Nuclear

    Renewable

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    Power Map : The colour-coded image of the Earth at

    night shows the use of electricity for Lighting is

    concentrated in industrialized regions(yellow)

    The red parts correspond to oil flares.

    Electricity Usage at Night

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    SINGAPORE

    KL

    IPOHPENANG

    TRONOH?

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    G.O.M. Offshore Platforms in Deepwater

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    Proven Global Oil & Gas Reserves

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    Including Malaysia

    PETRONAS a Fortune 500 Company **Has interest in 30 countries

    TOP TEN **

    @ Profit@ Return in

    Asset &

    Revenue

    44% of Malaysias Govt.

    revenue contributed by

    PETRONAS

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    Oil and gas fields/discoveries in Malay Basin

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    Example of Gas Field in an Oil Field

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    Malaysia Oil and Gas Fields

    Area Discovered Producing

    P.Malaysia 68 28Sarawak 44 16

    Sabah 28 9

    Total 140 53

    Area Discovered Producing

    P.Malaysia 89 9Sarawak 70 11

    Sabah 24 2

    Total 183 22

    Production Breakdown

    PM 42%

    Sabah8%

    Sarawak 50%

    MSIA/THAI JOINT

    DEVELOPMENTJOINT DEVELOPMENTMSIA/VIETNAM

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    Reserves

    Oil & Condensate

    Natural Gas

    Production

    (million barrels)

    (billion barrels)

    Reserve ( B.O.E )

    (billion barrels)

    (World Ranking)23rd

    14th

    Malaysia Oil

    and Gas

    PM 42%

    Sabah

    8%

    Sarawak 50%

    Production Breakdown

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    Corrective Initiative for Domestic Production Decline

    Reservoir & Field Development Perspective

    To compensate for Domestic Oil decline by

    corrective measures in Field

    Development

    improve recovery factor

    From 0.34 to 0.5

    EOR/IOR processes (WAG)

    find bypass oil by 4D

    Deepwater Contribution

    Cluster Development strategy

    Improving Recovery Factor

    600 Mbl/d

    9070 80 00

    Deepwater

    Contribution

    08

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    Major Oil Companies

    1. EXXON MOBIL

    2. Royal Dutch Shell

    3. TOTAL

    4. B.P5. Chevron

    6. Conoco Phillips

    7. Stat Oil

    8. REPSOL

    9. British Gas

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    National Oil Companies

    CNPCCNOOC

    PETROBRAS

    PETRONAS

    PEMEXONGC

    PETRAMINA

    NNPC

    PETROBANGLA

    PVDSA

    GAZPROM

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    Petroleum Economics

    5 10 15 20 Years

    US $

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    Sizes of Oil and Gas Fields

    G l i l i ld k

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    1985, P.D.O., Muscat, Oman

    Geological Field Work:

    Examining Exposed Rocks

    To Understand the Subsurface

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    Sedimentary Rocks

    Sedimentary rocksform from materials

    that are eroded from

    other rocks

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    Metamorphic Rocks

    Metamorphic rocksare rocks that have

    changed due to

    being heated and/orcompressed.

    Wh t T f R k R l t t

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    What Types of Rocks are Relevant to a

    Petroleum System?

    Mainly sedimentary rocks

    Sandstone for reservoir rocks

    Limestone for reservoir and source rocks

    Shale for source rocks and seals

    Evaporite (salt) for seals.

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    Sedimentary Basins of Malaysia

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    Mekong Delta, Thailand

    Niger Delta, NigeriaMahakam Delta, East

    Kalimantan, Indonesia

    Delta Satellite Images

    O i i T d D i i f

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    Origin, Transport and Deposition of

    Sediments

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    The Origin of Oil and Gas

    INORGANIC THEORYHydrogen and carbon are brought together under

    great pressure and temperature deep in the earthto form Petroleum

    ORGANIC THEORY

    Originated from the organic remains of plants andanimals buried in fine-grained sediments. The

    organic remains become kerogen then oil underhigh pressure and high temperature.

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    Source Rock

    Most commonly an organic-rich shale

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    Ganges Delta, India

    Turkmenistan

    Delta

    Ural Delta,

    Kazakhstan

    Bay of Bengal,

    India

    DELTA IMAGES

    S.E. ASIA BASIN EVOLUTION EARLY EOCENE (~55 MA) TO Curreny

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    Modified. from Scotese and PALEOMAP(2005) Courtesy Harry Doust

    ( ) y

    1) Collision of India plate moving eastward with Asia

    plate

    2) Further Collision with Australia plate moving

    Northward

    60 maPaleocene

    50 ma

    Early Eocene

    40 maLate Eocene

    30 maOligocene

    20 ma

    Early Miocene

    10 ma

    Late Miocene

    0 ma

    Present day

    60 maPaleocene

    50 ma

    Early Eocene

    40 maLate Eocene

    30 maOligocene

    20 ma

    Early Miocene

    10 ma

    Late Miocene

    0 ma

    Present day

    S E A i B i G

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    S.E. Asia Basin Geometry

    SEG Research Workshop, KL 2008

    Satellite View

    VARIOUS

    BASINS

    Pacific

    Deepwater

    Mature

    MALAY

    SARAWAK SABAH

    CONSON

    200 KMSUMATRA

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    Malay Basin Geology

    Malay basin is a prolific

    Petroleum Tertiary basin that

    has seen four decades of

    extensive E & P activity.

    It is an extensional deep

    (12Km) mature, NW trending

    basin. With dimension 500 X

    200 sq km

    Exploration is focused inMiocene stratigraphic. Units

    called Group E to K .

    Youngest to oldest.

    Courtesy PETRONAS

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    Petroleum System Processes

    120 F120 F

    350 F350 FGenerationGeneration

    MigrationMigration

    Seal RockSeal Rock

    ReservoirRockReservoirRock

    OilOil

    WaterWater

    GasCapGasCap

    EntrapmentEntrapment

    Source: AAPGSource: AAPG

    Petroleum System

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    Petroleum System

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    Trap Styles

    Fault

    Salt domeAnticline

    Pinch-out

    Unconformity

    Geochemistry for Source Rock Evaluation

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    Geochemistry for Source Rock Evaluation

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    Graphite

    Dead Carbon

    Temperature

    Organic

    Matter

    Fate of Organic Matter

    Humic

    Substances

    Kerogen

    methane

    oil

    Wet

    Gas

    ThermallyMaturedOrganicMatter

    Dry

    Gas

    Source Rock Maturation & Petroleum

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    Source Rock Maturation & Petroleum

    Generation

    The earthstemperatureincreases with depthin the earths crust.

    As organic matter is

    buried, it is heatedand transformed intokerogen, oil and gas.

    Most oil is producedbetweentemperatures of 60and 120 degrees C, ata depth range knownas the oil window.

    Kerogen Maturation Van Krevelen Diagram

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    HydrogenIn

    dex

    Oxygen Index

    Type I

    Type II

    Type III

    Type IV

    LEGEND BARS

    CO2, H2O

    OIL

    WET GAS

    DRY GAS

    NO HYDROCARBON

    POTENTIAL

    INCREASINGMATURATION

    Kerogen Maturation Van Krevelen Diagram

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    PlanningBlock

    Acquisition

    Frontier

    Exploration

    Prospect

    EvaluationDrilling

    Discovery Volumes Appraisal

    Reserve &

    Economic

    Reservoir

    Static ModelSimulation

    Production

    Forecast

    PVT

    RFT

    DST

    Development

    Plan

    Infill

    Drilling

    LIFE OF FIELD

    Exploration

    Appraisal

    Field Development

    EORFLOODING

    INJECTION SECONDARY

    RECOVERY

    PRODUCER &

    INJECTOR

    Secondary Recovery

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    The Role of Geoscientists:

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    The Role of Geoscientists:

    Finding and Monitoring Petroleum Resources

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    Gas bubbling in water

    GEOHAZARD IMAGES

    MALAYSIAN OFFSHORE

    Magic of Seismic in detecting Gas bubbling in water

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    MALAYSIAN OFFSHORE HAZARD

    (GAS BUBBLING NEAR PLATFORM)

    SINKING OF DRILLING RIG

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    DUE TO GAS HAZARD

    1 2

    3 4