Geology -- Metamorphic Rocks -- Ch. 6

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neyceee  on May 10, 2012

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Geology -- Metamorphic Rocks -- Ch. 6

Metamorphism
When rocks are subjected to enough heat, pressure, and fluid activity to change their mineral composition, texture or both
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Metamorphism When rocks are subjected to enough heat, pressure, and fluid activity to change their mineral composition, texture or both
Metamorphic Rocks Transformation of rocks by processes that occur beneath Earth's surface
3 Agents of Metamorphism Heat, Pressure, and Fluids
Heat Increases the rate of chemical reactions
Pressure Burying rocks subjects them to increasingly greater pressure
Lithostatic Pressure Pressure exerted on buried rock by overlying and surrounding rocks
Differential Pressure Stress is not equal in all direction
Fluid Activity The presence of fluids increase reaction rates forming new minerals
Contact Metamorphism Body of magma alters surrounding country rock
Country Rock Surrounding Rocks
Shock Metamorphism Rocks subjected to high levels of differential pressure and some heat by impact
Regional Metamorphism Occurs over a large area usually by intense temperatures and pressures within the deeper portions of the crust
Index Minerals Minerals that form in specific temperature and pressure ranges
Metamorphic Grade Characterizes the degree to which rocks have been metamorphosed; Unaltered, Low Grade, Intermediate, High Grade
Foliation Elongate or platy minerals arrange in a parallel fashion during metamorphism
Low Grade Metamorphism Fine Foliation
High Grade Metamorphism Thick Foliation
Slate Low-grade foliated metamorphic rock
Phyllite Similar in composition to, but coarser grained than slate
Schist Coarser grains than Phyllite
Gneiss High-grade metamorphic rock
Migmatite Formed from extremely high temperatures during metamorphism
Marble Composed of calcite or dolomite
Quartzite Forms under intermediate to high-grade metamorphic conditions under contact or regional metamorphism
Anthracite Forms from metamorphism of coals
Metamorphic Zones A belt of rocks showing the same degree of metamorphism
Isograds Separates metamorphic zones by mineral content
Metamorphic Facies A group of metamorphic rocks characterized by its own distinctive mineral assemblage formed under broadly similar temperature and pressure conditions

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