Sedimentary Petrology Flashcards

(58 cards)

1
Q

study of the processes of formation, transport, and deposition of material that accumulates as sediment in continental and marine environments and eventually forms sedimentary rocks.

A

Sedimentology

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2
Q

study of processes that erode, transport, and deposit sediments

A

Sedimentology

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3
Q

the study of the characteristics and origin of sedimentary rocks

A

Sedimentary Petrology

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4
Q

the study of the origin, relationship, and extent of rock layers (strata)

A

Stratigraphy

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5
Q

the study of rocks to determine the order and timing of events in Earth’s history: it provides the time frame that allows us to interpret sedimentary rocks in terms of dynamic evolving environments.

A

Stratigraphy

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6
Q

formed at low temperatures and pressure compared to igneous and metamorphic rocks.

A

Sedimentary rocks

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7
Q

rocks which form at or near the earth’s surface primarily through: Deposition of weathered material by water, wind, or ice (detrital, clastic, terrigenous), Direct inorganic chemical precipitation from water, or Precipitation by organic processes.

A

Sedimentary rocks

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8
Q

Sedimentary rocks are rocks that form at or near the earth’s surface primarily through?

A

Deposition of weathered material by water, wind, or ice (detrital, clastic, terrigenous)

Direct inorganic chemical precipitation from water

Precipitation by organic processes.

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9
Q

the physical breakdown (disintegration) and chemical alteration (decomposition) of rocks at or near the Earth’s surface.

A

Weathering

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10
Q

2 types of weathering

A

Physical / Mechanical weathering
Chemical weathering

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11
Q

These are processes that break the solid rock into pieces and may separate the different minerals without involving any chemical reactions.

A

Physical weathering

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12
Q

The most important agents in physical weathering

A

Freeze-thaw action
Temperature change
Salt dome intrusion
Root wedging
Wetting and drying
Organic activity
Unloading

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13
Q

Physical / Mechanical weathering prevails in?

A

cold climates, high altitudes, dry regions

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14
Q

repeated cycles of freezing and thawing, the expansion force of water as it freezes is sufficient to split any mineral or rock.

A

Frost wedging

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15
Q

Differences in temperature in a rock give rise to differential expansion (heating) and contraction (cooling).

A

Heating and cooling

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16
Q

The disruption of soil results in the swelling and contracting of soil particles.

A

Wetting and drying

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17
Q

The action of organisms, including animals and plants, reduces the size of rocks and minerals.

A

Organisms

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18
Q

the removal of thick layers of sediments overlying deeply buried rocks by erosion or uplift.

A

Unloading

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19
Q

Factors controlling weathering

A

Source Composition
Climate
Topographic Relief

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21
Q

Weathering where the dissolving of a solid in a liquid

A

Dissolution

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21
Q

Weathering where combination of a solid mineral or element with water.

A

Hydration

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22
Q

Weathering where both the chemical combination of oxygen with a compound and the change in the oxidation number of some chemical elements. it is usually used in mineral weathering

A

Oxidation and Reduction

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23
Q

the chemical process in which electrons are gained

A

Reduction

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24
Q

involves the transfer of charged atoms (ions) of calcium, magnesium, sodium, and potassium between waters rich in one of the ions and a mineral rich in another. This most effective in clay.

25
The removal of material by mobile agents such as water, wind, ice, or man
Erosion
26
Arrangement of minerals in Goldich Stability Series (from least to highest resistance)
Olivine, Ca-Felds, Pyroxenes, Amphibole, Na-feldspar, Biotite Mica, K-feldspars, Muscovite Mica, Quartz
27
Difference between Bowen's reaction series and Goldich Stability Series?
Bowen's shows
28
Transport media of Erosion
Air, Water, Ice, Gravity
29
Mode of Transport in Erosion
Rolling, Saltation, Saltation, Suspension
30
the clasts move by rolling along at the bottom of the air or water flow without losing contact with the bed surface
Rolling
31
the particles move in a series of jumps, periodically leaving the bed surface, and carrying short distances within the body of the fluid before returning to the bed again.
Saltation
32
turbulence within the flow produces sufficient upward motion to keep particles in the moving fluid more or less continually.
Suspension
33
Particles being carried by rolling and saltation are referred to as _____________ and the material in suspension is called _________________.
Bedload; Suspended load
34
Flow where all molecules within the fluid move parallel to each other in the direction of transport.
Laminar flows
35
Flow where heterogeneous fluids are thoroughly mixed
turbulent flows
36
Flow where molecules in the fluid move in all directions but with a net movement in the transport direction.
Turbulent flows
37
Flow where a heterogeneous fluid with almost no mixing.
Laminar flows
38
a dimensionless quantity that indicates the extent to which a flow is laminar or turbulent.
Reynolds number(Re)
39
Reynolds number is obtained by relating the following factors:
the velocity of flow (y), the ratio between the density of the fluid and viscosity of the fluid (n– the fluid kinematic viscosity) and a ‘characteristic length’ (l – the diameter of a pipe or depth of flow in an open channel)
40
These are the products of volcanic eruptions or the result of the breakdown of volcanic rocks.
Volcaniclastic sediments
41
This is material that is made up of particles or clasts derived from pre-existing rock
Terrigenous clastic material
42
makeup 20–25% of the sedimentary rocks in the stratigraphic record
Sandstones and conglomerates
43
makeup 60% of the sedimentary rocks in the stratigraphic record
mudrocks
44
any sedimentary rock containing over 50% calcium carbonate (CaCO3).
limestone
45
These are deposits formed by the precipitation of salts out of water due to evaporation
Evaporites
46
what are the other sediments and sedimentary rocks
sedimentary ironstone, phosphate sediments organic deposits (coals and oil shales) cherts (siliceous sedimentary rocks).
47
A widely used classification chat/ grade scale for classifying the diameters of sediments
Uden-Wentworth grain size scale
48
in udden-Wentworth scale, φ ______ as diameter ________.
increase; decrease
49
size of boulder in udden-Wentworth grain size scale
> 256 mm , -8 phi
50
size of cobbles in udden-wentworth grain size scale
16-128 mm; -4 - -8phi
51
size of silt in udden-wentworth grain size scale
0.063 to 0.0039 mm; 4 to 8 phi
52
size of pebbles in udden-wentworth grain size scale
4-16 mm; -2 to -4phi
53
size of granules in udden-wentworth grain size scale
2-4mm ; -1 to -2phi
54
size of sand in udden-wentworth grain size scale
2-0.063 mm ; -1 to 4 phi
55
Sedimentary rocks made of silt- and clay-sized particles. it is the most abundant
Mudrocks
56
Rock name for sedimentary rocks that is composed of gravel size (>2) sediments
Rudite
57
Rock name for sedimentary rocks that is composed of sand (0.065-2) size sediments
Aranite
58
Rock name for sedimentary rocks that is composed of Mud (<0.065) size sediments