Week 7 Flashcards
Parent rock (protolith)
The rock before metamorphism
Metamorphic grade
The degree to which a parent rock changes during metamorphism. It varies from low grade (temperature and pressure) to high
Recrystallization
The formation of new mineral crystals in a rock that tend to be larger than the original
Change in shape and size of grains without changing ID of mineral
Noecrystallization
Brand new minerals formed from protolith
Confining pressure
Stress that is applied in all directions
Differential stress
Forces that are unequal in all directions
CONVERGENT PB
Compressional stress
Differential stress that shortens a rock body
Shear stress
J
3 types of stress
Differential
Compressional
Shear
Texture (foliation)
Refers to any planar( flat) arrangement of mineral grains or crystals within a rock. Driven by compressional stress. Includes banding/ cleavage
Layers
Non foliation
Tends to be one type. No layers
Where deformation is minimal
Hydrothermal
Contact metamorphism
Changes in rock caused by the heat from a nearby magma body
Hydrothermal metamorphism
Chemical alterations that occur as hot iron rich water circulates through fractures in rock
Enhances recrystallization
Subduction zone (burial) metamorphism
High pressure low temperatures metamorphism that occurs where sediments are carried to great depths by a subducting plate
Types of metamorphic environments
Hydrothermal: low pressure, low to mid temp
Contact: low pressure, low to high temp
Regional: low to high temperature and pressure
Subd zone; high pressure low temp