SEDIMENTARY PETROLOGY (DETRITAL SEDS AND TEXTURES) Flashcards

1
Q

BOUNDARIES OF UDDENWENWORTH

A

265-2-0.0625-0.004

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2
Q

Earths surface covered by sediments and sed rocks

A

85%

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3
Q

Size shape, arrangement of sediments both its solid particles and void spaces between them

A

Texture

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4
Q

Uses of texture

A

1) Ability of sed rocks to store and transmit fluids
2) Susceptibility to Mass Wasting
3) Diagensis of Detrital seds

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5
Q

Wentworth udden scale is

A

Negative Base 2 Logarithmic Scale (-log2)

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6
Q

What did krumbein do to faciltate mathematical and statistical analysis of detrital sediments

A

Logarithmic Phi Scale equivalents

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7
Q

Phi fomula

A

Phi = -log2d

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8
Q

Coarse Fraction or grains

A

G and S

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9
Q

Fine Fraction or Matrix

A

M

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10
Q

In Folk classification of Detrital Sediments, these sediment or rcks contain 30% Gravel in their fraction

A

Gravel and Gravelstone

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11
Q

If gravel is more than 80%

A

Clast-suported Texture

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12
Q

Grvel that contains less than 80% of Gravel must have modifier of Sand- or mud-supported depending on sand:mud ratio

A

Matrix supported

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13
Q

Less than 30% Gravel and >1:1 Sand MudRatio

A

gS, gmS, (g)mS, (g)S, mS and S

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14
Q

Grave 5-30% >9:1 S:M

A

Gravelly Sandstone gS

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15
Q

Gravel 5-30% <9:1 S:M

A

Gravelly Muddy Sandstones gmS

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16
Q

Gravel <5%, >9:1 S:M

A

Pure Sandstone or Arenite (S)

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17
Q

Gravel <5% <9:1 S:M

A

Muddy Sandstone or Wackes (mS)

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18
Q

If either has traces of Gravel

A

Slighly Gravely Sandstone (g)S
Slightly gravelly Muddy Sandstone (g)mS

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19
Q

Gravel 5-30% <1:1 S:M

A

Gravelly Mud or Gravelly Mudrock gM

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20
Q

Gravel <5%, <1:9 SM

A

Pure Mud or Mudstone

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21
Q

Gravel <5%, >1:9 SM

A

Sandy Mud or Sandy Mudstone

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22
Q

Deviations of Folks SCZ

A

10-50-90 1:2 2:1

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23
Q

A graph which the wt% in each Phi Size class is plitted in the form of a vertical bar graph (Phi Size vs wt%)

A

Histogram

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24
Q

The best-fit line plotted in the histogram for the same data (Phi Size vs wt%)

A

Frequency Curve

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25
the cumulative weight percent of all size fractions coarser than and including the phi size fraction under consideration are plotted against the Phi size classes (Phi Size vs Cum Wt%)
Cumulative Frequency Curve
26
The most abundant particle size and is dertemined by histogram or frequency curve and is usually expressed in terms of the midpoint of the size class in which the largest wt% occurs (May pinakamaraming population)
Mode (ModeL - Popular)
27
when there are two size classes that are more abundant than those adjcent to them and thus have two modes
Bimodal Size Distribution
28
More abundant mode in a bimodal size disrtibution
Primary Mode
29
The particle size such that half the population is larger and half the population is smaller (GITNANG VALUE)
Median (Media=Center of attraction)
30
What corresponds to the Median?
Phi 50% in the Cumulative Frequency curve ung Phi size na intersecting with the pt in which 50%wt intersects or the abscissa of 50% wt
31
The average particle Size
Mean
32
Graphic Geometric Mean (GM)
(Phi16+Phi50+Phi84)/3 (values from CFC)
33
Similarity of particle size and increases when range or particle size increases
Sorting
34
What transportation media promote Sorting
Wind and Water
35
What transporation media forms very poorly sorte ddeposit
Glacial Ice and Mass Flows or Gravity
36
A steep cumulative cruve represet what type of sorting?
Well Sorted or Few size classes
37
Comptons Sorting Coefficient Formula
So=|Phi10%-Phi90%|
38
Inclusive Graphic Standard Deviation by Folk
So=[(phi84-Phi16)/4 + (Phi95-Phi5)/6.6]
39
Compton's Sorting Coefficient deviation (5 description)
1-3-5-7
40
Folks Sorting Coefficient deviaton (6 w/Moderately Well Sorted)
0.35-0.50-0.71-1-2
41
Between wind and water, which is a better sorting agent?
Wind
42
Divisios in a zingg diagram for grain shape
0.67 x and y
43
Clockwise
Sphere Prolate Bladed Oblate
44
Cylindrical or cigar shaped
Prolate (Kakain ng Apple)
45
Flattened cylinder or disklike shape
Oblate (Kakain ng Caimito)
46
Kinfe blade with one long, one intermeiate and one short axis
Bladed
47
Grains with long axis (a) is parallel to the flow of the current that deposited them
Prolate and Bladed
48
Grains which can show imbricaton
Large bladed and Oblate clasts
49
grains inclined in one directions usually in the up-current direction
Imbrication
50
Differentiate Sphericity from Roundness
Sphericity is the measure of the degree to which a particle approaches of a perfect shape that is being equat and spherical while Roundess is the degree of smoothing or curvature of grain edges
51
Formula for porosity
Ps=%Pore Space = (Vol of Pores/Total Rock Vol)X 100
52
Relationship of Porosity, Sorting ad Grain Roundess
Increases or Directly proportional
53
why is minera cementation patterns of prime important in the subsurface during petroleum and hydrological Explo
Because Mineral Cementation reduces porosity and thus reduced rock's ability to store fluids
54
What is permeability?
The rate of fluid flow through a rock
55
Darcy's Law
Q= A(Hc * delta H/l)
56
delta H/ L
Hydraulic Gradient
57
Hydarulic Conductivty formula
Density, effective permeability, gravity / viscocity
58
Levels for Assessing Textural Maturity
1. Mud Matrix Percent (>5% or <5%) 2. Sorting (well or poorly sorted) 3. Roundness (Angular or Rounded)
59
>5% mud sandstone maturity
Texturally immature
60
Why do water and wind laid deposits rarely immature?
Because wind and water keeps mud particles in suspension
61
<5% but poorly sorted
texturally submature
62
Implication of a texturally submature deposit?
rapidly decelerating or fluctuating flows that can deposit a range of sizes in a short time like River Systems (Braided and Levees), Storm deposits and turbidity Currents
63
<5% mud and well sorted
Deposited by wind and water and is well washed during slow accumulatio in beaches, sallow bars, and some strong channels
64
Rounded, <5% and well sorted
texturally Supermature
65
Angular <5% and well sorted
Texturally Mature
66
Refers to grain orientation and packing
Grain Fabric
67
In water laid sediments, grains may be oriented parallel or normal to the current direction
Prolate
68
IN water laid sediments, grain may show imbricated orienattion and overlap each other dipping upstream diection
Oblate
69
Packing of spheres which produces 48% porosity
Cubic Packing
70
packing with 26% porosity
Rhombohedral
71
SKEWNESS
Measures the symmetry of distribution uses smoothed frequency curve
72
Kurtosis
Peakedness of A frequency Curve