Sedimentary Rocks (Part 2 - Textures and Maturity) Flashcards

1
Q

Parameters for Textures

A

Grain Size
Grain Shape
Grain Orientation
Porosity
Permeability

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2
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
expressed as: 𝛷 = βˆ’π‘™π‘œπ‘”2d

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3
Q

The component of detrital sedimentary rocks that have particles sizes from sand to gravel.

A

Clasts

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4
Q

also called as Coarse Fraction

A

Clasts

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5
Q

Mud sized particles component of detrital sedimentary rocks.

A

Matrix

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6
Q

Also called Fine Fraction

A

Matrix

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7
Q

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

A

Central measure

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8
Q

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

A

Histogram

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9
Q

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

A

Frequency curve

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10
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

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11
Q

The most abundant particle size.

A

Mode

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12
Q

The average size of the particles

A

Mean

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13
Q

The average diameter of the particles

A

Graphic geometric mean (GM)

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14
Q

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

A

Sieving

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15
Q

Determines or gives information regarding the nature or maturity of a grain.

A

Grain Shape

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16
Q

2 Factors that affect shape

A

Lithology
Hardness

17
Q

Spheroid particles that have similar dimensions in all directions.

A

Equant

18
Q

Rod-shaped particles that have an elongate cylindrical that have on axis much longer than the other two.

A

Prolate

19
Q

Disk-shaped particles that have a flattened cylindrical or disk-like shape where two axes are shorter than the other.

A

Oblate

20
Q

Particles that have a flattened shape where the three axes have three different lengths.

A

Bladed

21
Q

The distribution of grain sizes present within a sedimentary rock.

A

Sorting

22
Q

A quick method of determining the phi size value for any percentile

A

Sorting coefficient

23
Q

A more complicated measure of sorting that involves finding values that are one standard deviation and two standard deviations above and below the mean.

A

Inclusive graphic standard deviation

24
Q

The volume of void space in a sedimentary rock.

A

Porosity

25
Q

The arrangement of grains in a rock.

A

Packing density

26
Q

The degree of how much fluids can pass through the materials.

A

Permeability

27
Q

The extent of how much sedimentary rock has undergone change starting from its parent material(s).

A

Maturity

28
Q

2 Ways to measure maturity

A

Textural and Compositional

29
Q

The degree of maturity that can indicate a sedimentary rock’s transportation history.

A

Textural Maturity

30
Q

The degree of maturity that measures the amount of components present.

A

Compositional Maturity

31
Q

Toblerone Sandstone Classification (for Detrital Seds)

A

Pettijohn Sandstone Classification (memorize boss)
pic: https://imgur.com/a/FS4ucTg