Diagenesis/Textures Flashcards

1
Q

Encompasses a suite of low temperature processes that affect sediments after their accumulation, typically after burial.

A

Diagenesis

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2
Q

A process of lithification that results from the expulsion of intergranular fluids caused by increases in confining pressure during progressively deeper burial.

A

Compaction

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3
Q

A process of lithification that occurs when subsurface fluids precipitate minerals in the spaces between grains that bind or cement grains to one another.

A

Cementation

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4
Q

What are the major cements of sedimentary rocks?

A
  1. Silica Minerals
  2. Carbonate Minerals
  3. Iron oxides and hydroxides
  4. Feldspars
  5. Clay Minerals
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5
Q

What is the most abundant silica cement?

A

Quartz

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6
Q

What is the most abundant cement in sandstones and gravelstones?

A

Carbonate minerals

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7
Q

What is the most abundant carbonate cement?

A

Calcite

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8
Q

What is the third most common cementing agent in sedimentary rocks?

A

Iron oxides and hydroxides

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9
Q

Chief iron oxide and hydroxide cements

A

Hematite, goethite, and limonite

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10
Q

Stages of Diagenesis

A

Eodiagenesis
Mesodiagenesis
Telodiagenesis

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11
Q

Early, shallow diagenesis that
occurs shortly after burial.

A

Eodiagenesis

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12
Q
  • Later, deeper diagenesis.
A

Mesodiagenesis

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13
Q

Still later, shallow diagenesis
that occurs as sedimentary rocks approach the surface due to erosion.

A

Telodiagenesis

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14
Q

Enumerate the texture parameters of sedimentary rocks.

A
  1. Grain Size
  2. Grain Shape
  3. Grain Orientation
  4. Porosity
  5. Permeability
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15
Q

A classification scheme that describes sediments’ particle sizes in epiclastic rocks. It also classifies particles sizes based on a logarithmic phi scale using the diameter (d)

A

Grain Size
Φ = -log₂d

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16
Q

A texture parameter of sedimentary rocks that determines or gives information regarding the nature or maturity of a grain.

A

Grain Shape

17
Q

What are the two factors affecting shape?

A
  1. Lithology
  2. Hardness
18
Q

Also known as the coarse fraction, is the component of detrital sedimentary rocks that have particles sizes from sand to gravel.

19
Q

Also known as the fine fraction, is the mud- sized particles component of detrital sedimentary rocks.

20
Q

A measure of particle population in an attempt to represent the typical particle size in the population.

A

Central Measure

21
Q

A bar graph that shows the weight percentage vs. phi values of clasts.

22
Q

A line graph that shows the weight percentage vs. phi values of clasts.

A

Frequency Curve

23
Q

A line graph that shows the cumulative weight percent of all size coarser than, including the phi size fraction under consideration, are plotted against phi size classes.

A

Cumulative curve

24
Q

A method of passing soil and sediment samples through a series of stacked mesh to determine the distribution of grain sizes.

25
**Spheroid particles** that have *similar dimensions in all directions.*
Equant
26
Rod-shaped particles that have an **elongate cylindrical** that have on *axis much longer than the other two*.
Prolate
27
**Disk-shaped particles** that have a **flattened cylindrical** or disk-like shape where *two axes are shorter than the other.*
Oblate
28
Particles that have a **flattened shape** where the *three axes have three different lengths.*
Bladed
29
The distribution of grain sizes present within a sedimentary rock.
Sorting
30
A quick method of determining the phi size value for any percentile, expressed as:
Sorting Coefficient S₀ =∣Φ₁₀−Φ₉₀∣
31
The arrangement of grains in a rock.
Packing Density
32
The degree of how much fluids can pass through the materials.
Permeability
33
The extent of how much sedimentary rock has undergone change starting from its parent material(s).
Maturity
34
The degree of maturity that can indicate a sedimentary rock's **transportation history.**
Textural maturity
35
The degree of maturity that measures the **amount of components present.**
Compositional Maturity