Use LEFT and RIGHT arrow keys to navigate between flashcards;
Use UP and DOWN arrow keys to flip the card;
H to show hint;
A reads text to speech;
10 Cards in this Set
- Front
- Back
origin of clasts for siliciclastic rocks
|
provenance
|
|
type of rock formed by the precipitation of minerals due to water. Either by chemical or biochemical processes.
|
Chemical Rocks
|
|
Most important minerals in Carbonate rocks
|
Aragonite, Low Magnesium Calcite, high Magnesium Calcite, and Dolomite.
|
|
2 types of carbonate clasts
|
intraclast, extraclast
|
|
sourced within the basin, carbonate equivalent to mud rip-ups
|
intraclasts
|
|
sourced from outside the basin.
|
extraclasts
|
|
Most common carbonate grain made of whole or fragmented fossils
|
skeletal particles
|
|
Type of carbonate grain that has a nucleus. When cut you can see layer. Forms in high energy environments
|
Ooids
|
|
A Rock made mostly out of Ooids
|
Oolite
|
|
grain that is not as spherical as an ooid and larger but about the same
|
Pisoid
|