Fasies n Deps Env

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    Depositional

    Environments,Facies, Facies

    Models andPaleogeograpy

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    DepositionalEnvironments

    Sediments accumulate in some environment ofdeposition or depositional environments

     These areas receive net deposition Erosion may occur, but deposition dominates Features of these depositional environments are

    preserved in the rock record Examples:

    Sediment texture

    Sedimentary structures (formed by processes in theenvironment) Fossils of organisms that lived in the environment

    Ancient environments can be reconstructedfrom the clues that are preserved in the

    sedimentary rocks

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    DepositionalEnvironments

    Classication! Continental " # Fluvial " Alluvial Fans, $raided

    %tream

      Meandering %tream

      # &acustrine  # Eolian

    '! (ransisional )%horelines* " # &obate )Delta*

      # &inear " Clastics

      Mi+ Clastic

    Carbonate

      Carbonates

    -! Marine " .eef 

      %helf 

      (urbidite  Pelagic

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    DepositionalEnvironments

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    Facies All the properties of a body of rock that allo0

    us to di1erentiate it from those above, belo0

    or laterally ad2acent to it roperties include

    !ithology " rock type, including color, etc# $omposition " mineral content  Texture " grain si%e, sorting, roundness Sedimentary structures Fossils

    Facies means aspect " same !atin root as &face' verall appearance of a rock body

    Facies are the products of depositionalenvironments

    Examples: lanar laminated ne *uart% arenite facies +ioturbated, poorly sorted muddy skeletal limestone facies $rossstratied arkosic conglomerate facies

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    Facies and -epositionalEnvironments

    •  The facies concept refers to the sum ofcharacteristics of a sedimentary unit,commonly at a fairly small (cmm) scale

    • !ithology

    • .rain si%e

    • Sedimentary structures

    • $olor

    $omposition• +iogenic content

    • !ithofacies (physical and chemicalcharacteristics)

    •+iofacies (macrofossil content)

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    Facies and -epositionalEnvironments

    • Facies analysis is the interpretation of strata interms of depositional environments (ordepositional systems), commonly based on a

    0ide variety of observations• Facies associations constitute several facies

    that occur in combination, and typically representone depositional environment (note that very fe0individual facies are diagnostic for one specic

    setting1)• Facies successions (or facies se*uences) are

    facies associations 0ith a characteristic verticalorder

    3alther4s &a0 (2345) states that t0o di6erentfacies found superimposed on one another and

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    http://www.gpc.edu/~pgore/geology/historical_lab/environmentchart.htm

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    Facies Model

    8n ideali%ed description of a facies

    $onstructed from modernenvironments and ancient rocks

    Serves as a 9orm for comparison

    Frame0ork for observation

    redictor of patterns

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    Facies Patterns

    .roups of facies commonly sho0patterns

    Pro+imal Facies (near the source)

    tend to be coarse grained Distal Facies (far from source) tend

    to be ner grained

     This pattern is displayed upstreamand do0n in rivers and onshore too6shore in coastal areas

    Facies are arranged according to

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     Transgressive and egressive systems can be identied byobserving facies and lithological

    changes in rock;sediment

     Transgressive " sediments ne

    up0ards, represent deeper 0aterenvironments

    egressive sediments coarsen

    up0ards, represents shallo0ing

    Facies $hanges

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    Facies Migration

    Facies migrate through space and time

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    Walther’s Law

    of the Correlation of Facies

    Only works where there are no unconformities Only facies that were laterally adjacent during

    deposition (result of laterally adjacent environments)can be stacked vertically

    Vertical arrangement of facies gives us information : Distribution of environments How environments migrated through space and time

    sed as a basis to build facies maps orpaleogeographic maps

     !ccurate time correlation of facies is essential "ime lines provide framework for correlation

    #io$events Volcanic ashes

    Other thin% uni&ue lithologies or marker beds

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    Representing Facies:Stratigraphic Sections

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    Deltas

    Marginal Marine Deposition

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    Ganges Delta, India

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    Mississippi Delta(partial), USA 

    Mi i i i D lt ( ti l)

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    Mississippi Delta (partial),USA 

    Drowning!

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    Niger Delta D Model

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    Modern DeltaS"en#iron$ents