8: Sedimentary Rocks & Processes Flashcards

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1
Q

How do sedimentary rocks form?

A

Deposition: laying down of material by a natural agent (air, water, ice, gravity) or by precipitation of solution
- Often occurs in sedimentary basins

Lithification:
compaction + Cementification = lithification
- Compaction: The process by which pressure reduced the volume of sediments due to a reduction in void space
- The process by which clastic sediments are converted to rock by the precipitation of mineral cement (calcite, quartz, iron oxides) between grains)

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2
Q

What are the three main categories of sedimentary rocks?

A
  1. Clastic (detrital)
    - starts as clasts, aka fragments or particles
    - sandstone, siltstone, shale, mudstone…
  2. Chemical (evaporites)
    - Formed by precipitation from solution
    - halite, gypsum, some limestones
  3. Organic (biogenic)
    - Formed from previously living organisms
    - Chalk, coal, and most limestones
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3
Q

Describe Clastic (detrital) sedimentary rock

A

Composed of fragments of weathered and eroded rocks, grains, and particles

The longer the rocks travel:
- the finer the grains
- the more rounded and less angular due to abrasion from transport

poorly sorted = well graded, you start with this

well sorted = poorly graded
you get this after a long transport

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4
Q

For Clastic Sedimentary Rocks, what are the 4 groups? Give examples for the major 2:

A

Mudrock
- mudstone: 75% silt and clay, not bedded
- Shale: 75% silt and clay, thinly bedded
- siltstone: More silt than clay

Sandstone
- Quartz sandstone: dominated by sand, >90% quartz
- Arkose: dominated by sand, >10% feldspar
- Lithic wacke: dominated by sand, >10% rock fragments, >15% silt and clay

Conglomerate
- pebbles to boulders, rounded clasts

Breccia
- Pebbles to boulders, angular clasts

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5
Q

Give me some characteristics of Shale, Mudstone, Sandstone, Conglomerate, and breccia:

A

Shale: splits easily along bedding and lamination

Mudstone: does not break in layers like shale

Sandstone: Dominated by sand sized grains that are cemented together

Conglomerate: rounded grains >2mm in a finer-grained matrix

(only diff is conglomerate is like rounded chocolate chips while Breccia is like chocolate flakes in mint ice cream)

Breccia: Angular grains >2mm in a finer-grain matrix

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6
Q

Describe Chemical (evaporites) sedimentary rocks

A

Precipitation of minerals from solution
- Often requires restricted basin in warm arid climates

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7
Q

What are some common evaporites?

A

Halite: NaCl (rock salt)

Gypsum (CaSO_4 2H_2O)
- used in “Gyprock” drywall

Speleothems: CaCO3
- precipitated in caves
Tufa: CaCO3
- precipitated from cold springs
Travertine: CaCO3
- Precipitated from hot springs

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8
Q

Describe Organic (biogenic) sedimentary rocks. Name Some:

A

They are the remains of living things.

limestone
chalk: Another calcium carbonate from plankton
Coal: Formed from the remains of vegetation, composed mainly of carbon (fossil fuels)

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9
Q

What is coalification?

A

Conversion of peat (organic soil) to sedimentary rock under pressure and temperature

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10
Q

What are fossils in sedimentary rock? What do they do?

A

Fossils are the preserved traces of animals, plants, and other organisms,

They help us identify and correlate sedimentary rocks at different sites

Also help us date rocks

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11
Q

What is sedimentary structures? Name all the layers:

A

Sedimentary structure is a feature formed during deposition that gives clues to the environment and the time and place:

TOP
- Planar bedding
- current bedding showing cross lamination
- ripple marked bedding
- imbricate (overlapping) fossil shells)
- Graded bedding
- Cut-and-fill bedding
BOTTOM

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12
Q

What is Bedding?

A

A layer of sediment or sedimentary rock with a recognizable top and bottom called a bed

The boundary between 2 beds is a bedding plane

A series of beds that is distinct from beds above and below (and thick enough to be shown on a map) is called a formation

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13
Q

What can ripples in sedimentary structures tell us?

A

There are symmetric and asymmetric ripples:

symmetric: still water like beach

Assymetric: a direction was prefered, like ripples in a river bed or wind in a desert

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14
Q

What are facies?

A

They are a distinct rock unit that forms under certain conditions of sedimentation, reflecting a particular process or environment

Here, vertical and lateral differences reflect changes in conditions over time and space

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15
Q
A
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