Final Rev Flashcards
evaporates
gypsum - anhydrite
gypsum alters to anhydrite by dehydration
3 types of gypsum
nodular “network mesh of gypsum that grew in a muddy matrix” “chickenwire texture” (at surface)
massive “lacks internal structure”
laminated “alternating gypsum and clay/silt/mud” (seasonal)
halite
shallow water evaporite mineral
sucession of evaporite minerals
remaining seawater:
50% - carbonate
20% gypsum
10% halite
5% Mg and K salts
chert
silica rocks that form from precipitation
biology is important for the formation of chert
chert textures
granular microquartz
chalcedony
megaquartz
3 critters that make chert
diatoms
radiolarans
siliceous sponge spicules
2 basic types of chert
bedded (layers of pure chert, biological)
nodular (irregular, diagenetic)
varieties of chert
flint, jasper, novaculite, porcelanite, siliceous sinter
iron bearing rocks
> 15% iron
SiO2 40%
Fe 30%
-old
2 types: iron formation, ironstone
ironstone
nonbanded, commonly oolitic, non cherty
iron formation
well banded, interbanded, resemble limestone, cherty
phosphorite (def)
> 15% phosphorous
resemble limestone texture
phosphatization replaces skelatal and other carbonate grains on shallow subsurface
phosphorites (types)
nodular (authigenisis or diagenisis)
bioclastic (accumulation and burial of organic debris)
pebble bed
guano (bird poop)
humus
decay of plants
peat
precursor of coal
sapropel
fine organic material in lakes, lagoons, marine basins (e.g phytoplankton, spores, zooplankton)
coals
-carbonaceous compacted plant remains
-readily combustible
rank of coals
lignite
subbituminous
bitumionous
anthracite
classification for carbonaceous rocks
Catagenesis
Process by which kerogen heated to form petroleum >1000m,50-1206
Kerogen
Precursor to petroleum between sapropel and petroleum
Bitumen
Hydrocarbons in a semi or solid state eig tax
Req- for carbonate formation
- Lack ov low siliciclastic input
- Warm tropical or subtropical
- Light