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New Jersey granite gniess
Some of the oldest rock in the world located in New Jersey

Contact metamorphism
occurs near molten magma/lava
High temp
Low pressure

Regional metamorphism
high temp and high pressure
Continental crust collision
Subduction zones
Volcanic arcs

Dynamic metamorphism
Involves faulting and pressure
Occurs over broad belts of crust
Continental crust collisions
Subduction zones
Volcanic arcs

Shock metamorphism
Describes the effect of shockwave related deformation and heating during impact events

Hydrothermal metamorphism
Dissolved mineral-rich water released from a magma chamber interacts with the surrounding rocks as it cools, changing both the chemistry of the water and the chemistry of the rocks.

Metasomatism
hydrothermal alteration that involves large amount of externally-derived fluid from magma flushed through the system at the high pressures and temperatures and substantially alters the chemical composition of the rock.

The approximate temperatures and pressures of metamorphic grades are illustrated below

Metamorphic isograd
An isograd is a plane of constant metamorphic grade in the field; it separates metamorphic zones of different metamorphic index minerals
Metamorphic Facies
A metamorphic facies is a set of metamorphic mineral assemblages that were formed under similar pressures and temperatures

Stress
A force applied to a surface and it varies with increasing temp and depth in the earth
Uniform stress
Applied equally from all directions
Foliation
Parallel fabric in regionally metamorphosed rocks
Metamorphic stress


Phyllite
Wavy, glossy sheen, with large mica flakes but similar to a slate
Migmatite
Mixed rock of Felsic composition and forms near large granite intrusions.
Represents transition between igneous and metamorphic rocks

My limits
Mixed rock formed during dynamic metamorphism

Marble
Metamorphosed limestone or dolostone

Skarn
Formed during the contact metamorphic zone of igneous intrusion

Quartzite
Metamorphosed sandstone

Hornfel
Contact metamorphic rock that has been baked and hardened by the heat of intrusive igneous masses

Amphibolite
Amphibolites are rocks composed mainly of amphibole and plagioclase feldspar, with little or no quartz

Serpentinite
A serpentinite is a hydrothermally metamorphosed mafic rock that is abundant on the ocean floor, but also occur in continental crust through interaction of mafic rocks with groundwater