METAMORPHIC PETROLOGY (FUNDAMENTALS) Flashcards
This refers to predominantly solid state mineral and/or textural changes to preexisting protoliths
“to change form” a process that leads to changes in mineralogy, texture, and sometimes chemical composition
Metamorphism
Agents of metamorphism
1.Temperature,
2.Pressure,
3.chemically active fluid
4. Differential stress*
Types of metamorphism which results from INCREASING T and P consitions overtime w/c involces recyrstallization and neocrystallizaton to transform minerals in accordance with equilibrium
Prograde Met
Type of Metamorphism which results to DECREASE T and P so that lower T/P minerals OVERPRINTS unstable ones with the AID OF VOLATILES
Retrograde Met
Type of Met which progresses incrementaly from slight changes
Low-grade Met
Type of Met which progresses incrementaly showing substantial changes
High-grade Met
Determine if its Retrograde or Prograde
1. Neocrystallization
2. Overprinting with aid of volatiles
3. Recrystallization
- PM
- RM
- PM
Differentiate Prograde and retrograde metamorphism
Prograde metamorphism results from increasing temperature and pressure conditions over time which involves recrystallization and neocrystallization to transform minerals in accordance with equlibrium meanwhile Retrograde metamorphism occues when temp and pressure conditions decreases so that lower temp/press minerals overprints unstable minerals with the aid of volatiles
This involves the use of mineral assemblages and their deformation chatacteristics to infer peak PT conditions of metamophism
Geothermobarometry
This mineral occurs in LT HP in subduction zones
Glaucophane
lower limits of metamorphism
Diagenesis
150-200 deg cel
<3kbar
10km depth
Temp limit of diagenesis
150-200 deg cel
Pressure limit of diaganesis
<3Kbar
Depth limit of Diagenesis
10 km
Upper limits of metamorphism
Anatexis (Partial melting) (600-800deg)