Section 7- Sedimentary Rocks Flashcards
Sedimentary Rock Formation
Deposition and lithification
Deposition
laying down of material by a natural agent (air, water, ice, gravity)
or precipitation from solution
lithification
Compaction
-process which pressure reduces the volume of sediment due to a reduction in void space
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Cementation
-process by which clastic sediment are converted to rock by precipitation of mineral cement (calcite,quartz,iron oxides) between grains
-crystallizing in pore space to hold sediments together, happens when water flows through pores between sediments, ions in the water combine to form crystals to fill the pores and hold sediment together
Sedimentary Rock Types
clastic (detrital)
- starts as clasts(fragments or particles)
-form from fragments of other rocks that have been weather, eroded, etc and overtime compacted and cemented together
Chemical (evaporites)
-formed by precipitation from solution
Organic (biogenetic)
-formed from previously living organisms
Clastic (detrital)sedimentary rocks
composed of fragments of weathered and eroded rocks that are compacted and cemented together
3 main types of clastic rocks
mudrock
-smaller particles, silt and clay
sandstone
-dominated by sand
conglomerate
-pebbles to boulders, rounded clasts
breccia
-pebbles to bouders, angular clasts
chemical (evaporites) for sedimentary rocks
precipitation of minerals from solution
-often requires restricted basin in warm climate
-halite and NaCl
organic (biogenic) sedimentary rocks
remains of living things
-limestone
-coal
sedimentary structures:
bedding and ripples
Bedding
-layer of sedimentary rock with a recognizable top and bottom
-boundary between two is called bedding plane
Ripples
-symmetrical ripples formed by waves (both directions)
-asymmetrical ripples formed by wind or river (current in one direction) (gentle ->steep slope indicate current direction)
Facies
a distinctive rock unit that forms under certain conditions of sedimentation, relfecting a particular process or environment
Walthers Law
a vertical sequence of facies reflects a lateral change in depositional environment
Marine Transgression
sea level rises
depositional environments migrate towards land
marine sediments (shale and limestone) deposited on top of continental sediments (sandstones)
(Coarse to fine sediment)
Marine Regression
sea level falls
depositional environments migrate toward sea
continental desiment(Sandstone) deposited on top of marine sediments (shales nad limestones)
(Fine sediment to coarse)
Angular unconformity
Younger sediment rets upon the eroded surface of tilted or folded older rocks
Angular unconformity
Younger sediment rets upon the eroded surface of tilted or folded older rocks