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Take an existing rocks and subject it to additional heat and pressure and you change it to a metamorphic rock During additional heat and pressure you get very fine grains and a layered appearance to them. |
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Pressure is applied to the protolith, which causes it to shear or bend, but not break. Temperatures must be high enough that brittle fractures do not occur, but not so high that diffusion of crystals takes place |
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Forces are applied equally in all directions |
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Forces are unequal in different directions Convergent Plate Boundaries |
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Lines in the rock due to high pressure |
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Rock or Slaty Cleavage Schistosity Gneissic Texture |
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Rocks split into thin slabs when hit with a hammer |
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Foliation characteristic of coarser grained metamorphic rocks |
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Dark and light silicate minerals are separated giving he rock a banded appearance |
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Metamorphic rocks that do not exhibit foliation |
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Contact or Thermal Hydrothermal Regional Burial and Subduction Zone |
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Used to determine the degree of metamorphism a rock has experienced |
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A mineral that is identical to another mineral in chemical composition but differs from it in crystal structure |
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