Classification
Exogenic Endogenic
"Clastic" chemical and(fragmental) biochemical
(detrital) sediments
Cataclastic Hybrid sediments organic residues
till, tillite and rocks coal, etc.
(glacial) calcareous (CaCO3)
shale
Pyroclastic carbonaceous (C)
Tuff, ash shale
(volcanics)
Precipitated
Residues sediments and
"soils" rocks
Epiclastic non evaporites
sediments evaporites
washed
residues limestones halite
8% dolomites gypsum
phosphorites anhydrate
chert
iron-bearing
sediments
coarse fine
(resistates) (hydrolysates)
Conglomerates shale (siltstone)
Sandstones 81% of
11% of sedimentary
sedimentary rocks
rocks
Identification of Sedimentary Rocks
1. Mineral species and grain size (Wentworth Scale)
60% Feldspars
plagioclase
orthoclase
15% Quartz
calcite (CaCO3)
rock fragments
mica
hornblende
2. Texture - relationship of grains to one another
A. Contacts
1. Floating Diagenesis
increasing
compaction
compression
cementation
2. Point
3. Long
4. Concave - Convex
5. Sutured
Metamorphism
3. Rounding
a. Angular
b. Sub-angular
c. Sub-rounded
d. Rounded
4. Sorting - scatter of grains within a sediment or sedimentary rock
well sorted - small range in grain sizes
poorly sorted - wide range in grain sizes
Sediment or Sedimentary Rock Classes
Immature Mature
Sorting wide range of small range of
sizes - dirty sizes - clean
Rounding angular to sub-rounded to
sub-angular rounded
Mineral least resistant more resistant
Composition plagioclase quartz, chert
clays, mica k-feldspars
olivine, pyroxene
Texture floating point long, concave-
convex, sutured
Statistics