Slides 3b Clastic Sedimentary Rocks 2010

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Clastic Sedimentary Rocks

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  • Robert Gordon University 1

    Lecture 3b: Dynamic Earth: Clastic

    Sedimentary Rocks

    Sedimentary rocks = reservoir rocks, seals and source rocks

    ENM200: Dynamic EarthDr Bryan T Cronin ([email protected])

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    Clastic sedimentary rocks (e.g. sandstones, mudstones, conglomerates.are made of material eroded from one place then transported to and depositedin another.

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    The Rock CycleThe RockCycle

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    Mechanical weathering

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    Mechanical weathering: frost wedging

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    Mechanical weathering:material is eroded (usuallyby frost wedging) then movesprogressively down the drainage system (rivers etc)

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    Chemical weathering

    Chemical weathering includes dissolution (particularly of limestones) and rusting (oxidation)

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    Chemical weathering of these sandstone blocks has attacked the cement between the grains, so that they become loose and fall out. The sandstone is more strongly cemented along closely-spaced beds (sand layers) and the sides of small joints or cracks in the rock. The overall effect is to produce a pock-marked surface which is sometimes called honeycomb weathering.

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    Weathering of different materials

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    High porosity (x43 on A4)

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    Low porosity (x31 on A4)

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    Conglomerate:

    Dunnottar Castle, Stonehaven,Aberdeenshire

  • Robert Gordon University 17Polymict Conglomerate

  • Robert Gordon University 18Litharenite (sandstone)

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    Kimmeridge Clay mudstones (grey and limestones (yellow), at Kimmeridge Bay, Dorset, England. This is the main oil-prone source rock of the North Sea

  • Robert Gordon University 20Mudstone under the microscope

  • Robert Gordon University 21Biosparite

  • Robert Gordon University 22Diapric anhydrite

  • Robert Gordon University 23Triassic Anhydrite

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    Sedimentary structures

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    Fluvial

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    SANDSTONE RESERVOIRS

    Introduction to environment section:

    Depositional Environments and a simplified classification

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    Depositional Environment

    ContinentalAeolianAlluvial fanFluvialLacustrineGlacial

    MarineMarginal/ParalicShelfSlopeBasin

    Controls on the size, shape and production characteristics of reservoir bodies

    Major effects on reservoir quality distribution: Porosity Permeability Net to Gross Ratio Connectivity/Compartmentalisation

    Identification in the subsurface, use of well logs, cores and cuttings

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    Sedimentary Environments

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    Sandstone Reservoirs Alluvial Fan

    Schematic model

    Modern Example

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    Sandstone Reservoirs - FluvialBraided River Meandering River

    Outcrop

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    Braided River log response (subsurface)

    Sandstone Reservoirs - Fluvial

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    Sandstone Reservoirs - Lacustrine

    Schematic

    Pyramid Lake, Nevada

    We will examine lacustrine environmentsprimarily in association with alluvialfans and fluvial sandstone reservoirs

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    Sandstone Reservoirs - Lacustrine

    Eocene Green River Fm., Utah, USA

    SOURCE ROCKS

    Lacustrine algal carbonate

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    Sandstone Reservoirs Aeolian Modern

    Analogue for Southern North Sea Rotliegend (Permian) Gas Fields

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    Sandstone Reservoirs Aeolian subsurface: Leman Field, southern North Sea

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    Sandstone Reservoirs - DeltaicSchematic Delta Components

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    Sandstone Reservoirs Littoral

    Barrier Island

    Galveston Island, Texas, USA

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    Sandstone Reservoirs

    Littoral

    Map of Aux Vases foreshore and tidal channel sands, Carboniferous, Illinois, USA

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    Idealised Turbidite Depositional Sequences

    Sandstone Reservoirs Deep Marine

    Retrogradational fans Progradational fans

    Turbidite:Bouma Sequence

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    Reservoirs: A Simplified Classification

    Aeolian

    FluvialLacustrineGlacial

    shelfslope

    basin

    Turbidites, Talus, Gravitydeposits

    littoral

    deltaAlluvial Fan

    5 PRINCIPAL TYPES OF RESERVOIR

    5 PRINCIPAL TYPES OF DEPOSITIONAL ENVIRONMENT

    Sandstone, Limestone, Chalk, Dolomite, Others

    Continental, Marine Littoral Deltaic, marine Littoral non-Deltaic, Marine Shelf,Deep-marine

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    Lecture 3b: Dynamic Earth: Clastic Sedimentary RocksThe Rock CycleMechanical weatheringMechanical weathering: frost wedgingChemical weatheringWeathering of different materialsHigh porosity (x43 on A4)Low porosity (x31 on A4)Sedimentary structuresFluvialSANDSTONE RESERVOIRSDepositional EnvironmentSedimentary EnvironmentsSandstone Reservoirs Alluvial FanSandstone Reservoirs - FluvialSandstone Reservoirs - LacustrineSandstone Reservoirs - LacustrineSandstone Reservoirs Aeolian ModernSandstone Reservoirs Aeolian subsurface: Leman Field, southern North SeaSandstone Reservoirs - DeltaicSandstone Reservoirs LittoralSandstone Reservoirs LittoralSandstone Reservoirs Deep MarineReservoirs: A Simplified Classification