Title: Siliciclastic Sedimentary Rocks
1Siliciclastic Sedimentary Rocks
Distribution Classification
2Three Major Types of Siliclastic Sedimentary Rocks
Conglomerates
Mudrocks
Sandstones
3Conglomerates Breccias
Sandstones
Mudstones
4Conglomerates
5Generally repesents only a short transport
distance
Cgl 1
Cgl 2
Cgl 1
6Breccias Angular clasts
Mud-supported
Cement-supported
7Breccias
Clast-supported, point-to-point contact
Mega-Breccia, Death Valley, CA
8Generally repesents only a short transport
distance
Cgl 1
Cgl 2
Cgl 1
9Intraformational Conglomerate
10Distribution of sediments across the floodplains
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13Classification of Conglomerates An example
14Sandstones
15Sandstones consist of Grains, Matrix, Cement,
and Porosity
16Three Primary sorts of Grains
Quartz
Feldspars
Lithic Fragments
17Sandstone Maturity
Texturally and compositionally immature . Mainly
unstable grains, poor sorting, angular grains.
Texturally and compositionally mature. Mainly
quartz grains, well sorted, rounded grains
18Goldich Reaction Series
19Sandstone mineralogy related to time, climate
and transport distance
IMMATURE
Lithics, Feldspars Quartz
SUBMATURE
Feldspars Quartz
Quartz Feldspars
Quartz Feldspars
SUBMATURE
MATURE
SUPER MATURE
Quartz
Quartz
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21Sandstone Classification Systems The Pettijohn
(1975) System
22Lithic Arenite
Quartz Arenite
Mature/Distant/Old
Immature/Proximal/ Young
23Arkose
Submature/ Proximal-Distal/ Moderately old
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28Sandstone Classification Systems The Pettijohn
(1975) System
29Graywackes
Q
Quartz wacke
5
Arkosic wacke
Lithic wacke
F
50
R
30Graywackes
31Sandstone Classification Systems The Pettijohn
(1975) System
32Mudstones/Shales
- Consists of silt and clay-size minerals
- Quartz
- Phyllosilicates
- (a) Kaolinite
- 11 mineral
- (b) Smectite
- 21 mineral
- (c) Illite
- 21 mineral
Very fine particle size and cohesiveness of
sediments results in a sheet-like appearance.
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37Diagrammatic Representation of Illite
4Si
6O
Various Cations, Commonly K
6O
3Si1Al
4O, 2(OH)
6Al
4O, 2(OH)
4Si
6O
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45Distribution of Siliciclastics
Conglomerates Arenites
SUBMATURE
Arenites
Arenites Graywackes
Graywackes Mudstones
46Provenance
47Burial
Lithification 1. Cementation 2. Compaction 3.
Loss of Perm- iability 4. Loss of Poros-
ity 5. Mineralogical Alteration
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50Pressure solution/cementation
51Siliceous cements
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