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Types of Metamorphism

Contact, regional,, metasomatism

Contact metamorphism

Pre-existing rock gets "baked" under relatively low pressures from magma cooling underneath it - forms an "aureole" in adjacent rock

Regional Metamorphism

Pre-existing rock is subjected to heat and pressure on a regional scale - can result in different "grades" of metamorphism"


Rocks get squeezed closer and closer together as the tectonics plates get closer and closer (associated with mountain building)

Foliation

In response to pressure, platy minerals line up


If pressure is uniform, platy minerals don't align

Granoblastic texture

Non-foliated

types of granoblastic rocks

Quartzite, marble



Metasomatism

Occurs when fluids react with pre-existing rock and alter chemical composition - sometimes the fluid even gets involved in the rock

Example of Metasomatism

Olivine + H2O -> Serpentine

Highest to lowest grade of metamorphism

Slate -> Phyllite -> Schist -> Gneiss

Fossils in Metamorphic Rock?

Fossils are often obliterated or deformed