Alterations Flashcards
Type of alteration where rocks turn green
Propylitic Alteration
Propylitic Alteration occurs at relatively ______________
Low Temperature
Propylitic Alteration is characterized by what mineral(s)?
Chlorite, Epidote, Antinolite
Usually form from decomposition of Fe-Mg bearing minerals
Propylitic Alteration
Forms from decomposition of feldspars.
Sericitic Alteration
In Sericitic Alteration, rocks are altered into what mineral?
Sericite
An alteration consist of sericite and quartz
Phyllic Alteration
High temperature type of alteration which results from potassium enrichment
Potassic Alteration
Minerals associated with Potassic alteration
Biotite, K-feldspar, Adularia
Potassic alteration can occur in?
(a) Deep plutonic environment
(b) Shallow volcanic environment
This mineral is formed in shallow volcanic environment
Adularia
Can form before complete crystallization of magma
Potassic Alteration
A relatively high temperature type of alteration where albite or sodic plagioclase are formed.
Albitic
It’s presence usually indicates Na Enrichment
Albitic Alteration
A process by which Ca-bearing plagioclase feldspar is altered to a characteristic assemblage of saussurite
Saussurotization
A type of alteration where pyroxene is changed into amphibole
Uralitization
A type of alteration where secondary silica (SiO2) is added
Silicification
It is one of the most common type of alteration and occurs in many different styles
Silification
Silification can occur in ________ temperature
Wide range
General term for addition of silica by forming any type of silicate mineral
Silication
Formation of a type of rock called greisen
Greisenization
General term for the addition of any type of carbonate mineral
Carbonatization
Type of alteration that is closely associated with certain hot springs environment.
Alunitic
The presence of this mineral suggest high SO4 content
Alunite
Presence of alunite suggest ______
High SO4 content
Low temperature, acidic alteration
Argilic
Type of alteration that includes the bleaching out of feldspars
Argilic alteration