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Published byChristian Sedwick Modified over 9 years ago
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Metamorphic rocks form when the crust is exposed to rising pressure and temperature conditions. What processes can raise the pressure and temperature of the crust?
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Metamorphic Rocks Are Composed of Sedimentary, Igneous, or Metamorphic Minerals that Have Recrystallized. Marble from Carrara, Italy
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Pre-existing sedimentary, igneous, or metamorphic rock changed to a new assemblage of minerals. Result of solid-state recrystallization of “parent rock” due to changing crustal conditions. What Is Metamorphic Rock?
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Rocks Evolve through a Sequence of Metamorphic Grades …
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… conveniently “indexed” by Index Minerals
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Regional Metamorphism = stress = foliation
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Shale is parent rock (protolith) Foliated texture is produced by directed stress related to regional metamorphism
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Slate Fractures along parallel planes. Phyllite Parallel mineral arrangement. Schist - parallel to sub-parallel arrangement. Gneiss Minerals segregated into bands.
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Contact Metamorphism = thermal
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Limestone changed by contact metamorphism into marble and various types of minerals Contact metamorphism forms Quartzite Hornfels Marble
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Quartzite Hornfels Anthracite Marble Metaconglomerate Nonfoliated rocks may develop during regional or contact metamorphism
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In addition to heat and pressure, chemically active fluids transport heat and promote recrystallization
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Identify where you would find metamorphic rocks and their type.
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Plate Movement Powers the Rock Cycle Igneous Granite/Rhyolite Diorite/Andesite Gabbro/Basalt Peridotite (Komatite) Sedimentary Conglomerate/Breccia Sandstone Shale Limestone Coal Metamorphic Slate Phyllite Schist Gneiss Hornfels Marble Quartzite
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