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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