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IX Metamorphic Rocks A B C D E Evidence of metamorphism The recipe for metamorphism Prograde metamorphism of shale Classification of Metamorphic Rocks Metamorphism and Plate Tectonics The Rock Cycle Geological Materials Transformation Processes Rock Metamorphism (Icreased & P) T Metamorphic rock Partial Meltig Magma Metamorphism Metamorphic Rocks Defiitio: Re-crystallization of minerals While still solid Into minerals that are stable at different temperatures and Different pressures (Usually progressively higher temperatures and pressures) A Evidence of Metamorphism E.g., Sedimetary Rocks Made of minerals derived from weathering of a parent rock Stable at atmospheric temperatures and pressures (low T & P) Originally horizontal, continuous and uniform layers Bet (deformed) layers Fig 8-1, p 168 Evidence of Metamorphism Differetia l pressure “squashes” rock ad icluded features Flatteed Pebbles Evidence of Metamorphism Crystallie Texture Minerals tightly interlocking due to recrystallization under pressure Evidence of Metamorphism New mieral assemblages E.g., Shale: Clay mierals (some quartz) Metamorphism Forms Schist: Mica, Feldspar ad other silicate mierals B Recipe of Metamorphism Paret Rock Even though minerals will change Most elements are provided by parent rock Except water and some dissolved ions Shale Schist B Ingredients of Metamorphism Temp (ºC) 500 1000 A B C Icreased Temperature (high geothermal gradiets) Minerals stable at lower temperatures converted to minerals stable at higher temperatures Metamorphic Rocks of other Parent Rocks Quartz Sadstoe Graular quartz Crystallie quartz Quartzite Metamorphic Rocks of other Parent Rocks Basalt Amphibole Graite Schist Geiss Uiform texture Foliatio (schistosity ad geissic badig) Where does Prograde Metamorphism occur? Temp (ºC) 600 1200 A B C Where temperatures ad pressures are progressively icreased: Subductio zoes ad Moutai belts Regioal Metomorphism at Coverget plate boudaries Prograde Metamorphism in Mountain Belts Northeastern North America Metamorphic Grade High Northwestern Africa Low For each rock type discussed kow: Grain size (rounding and sorting if sedimentary) Texture (clastic or crystalline) Other characteristics Various types of metamorphic foliation Various sedimentary structures Environment of formation History of formation Rock Classification Review for Exam Reading the Grand Canyon The Grand Canyon Fig 8.16 The Grand Staircase Coconino Sandstone Redwall Limestone Sedimentary Rocks Intrusive Igneous Metamorphic Bright Angel Shale Grand Canyon Pink Granite Vishnu Schist (and gneiss) The Grand Staircase Fig 8.16 Eastern Zion National Park Checkerboard Butte Zion National Park Vishnu Schist and Pink Granite [...]... resultig i silicic veis if itrusive igeous rock Fig 7.12 Metamorphic Rocks of other Parent Rocks Limestoe Marble Bioclastic calcite Crystallie calcite Metamorphic Rocks of other Parent Rocks Quartz Sadstoe Graular quartz Crystallie quartz Quartzite Metamorphic Rocks of other Parent Rocks Basalt Amphibole Graite Schist Geiss Uiform texture Foliatio (schistosity... Mica ad Quartz Medium-grade metamorphic Mierals stable uder medium grade metamorphic T&P Causescoditios appear: Garet, amphibole ad biotite mierals to Schistosity due to aligmet of grow platy ad eedle likemierals Prograde Metamorphism of Shale 4: High-Grade Metamorphism Geiss Course graied Feldspar, Quartz, Amphibole, Biotite Fig 7.12 High-grade metamorphic T&P Causes Mierals... to grade metamorphic coditios separate ito appear: feldspar bads Geissic badig bads of dark ad light mierals Prograde Metamorphism of Shale 5: Very HighGrade Metamorphism ad partial meltig Migmatite Silica rich mierals melt first (quartz ad feldspar) Formig silicic magma Ijected ito fractures resultig i silicic veis if itrusive igeous rock Fig 7.12 Metamorphic Rocks of... Metamorphism of Shale (and the classification of metamorphic rocks) Shale: Fie graied Clay (ad quartz) Mierals stable uder low T&P (atmospheric) Compactio due to accumulatio of sedimet Fissility alog lamiatios Water boud i crystallie structure of clay Prograde Metamorphism of Shale Me tamorphic grade 1: Low Grade Rock: Slate Low grade metamorphic T&P (Water is expelled from crystallie... from crystallie structure of clay) Mierals stable uder low grade metamorphic coditios Fie graied Mieral compositio : Mica (ad Quartz) Foliatio: Slaty Cleavage due realigmet of platy mierals to Prograde Metamorphism of Shale 2: Medium-Grade Metamorphism Phillite Courser graied Mica ad quartz Medium-grade metamorphic T&P Causes Slaty cleavage becomes mierals to grow rippled... Lithostatic Pressure as rocks are buried Differential Pressure at convergent plate boundary Fig 8-3, p 169 Results of Stress (Pressure) Differetial Pressure Parallel aligmet of platy mierals (e.g., micas) ad eedlelike mierals (e.g., amphiboles) Forms Foliatio Ingredients of Metamorphism 4 Additio or removal fluids (ad elemets) of Water (and other fluids) within rocks and minerals... Coverget plate boudaries Prograde Metamorphism in Mountain Belts Northeastern North America Metamorphic Grade High Northwestern Africa Low For each rock type discussed kow: Grain size (rounding and sorting if sedimentary) Texture (clastic or crystalline) Other characteristics Various types of metamorphic foliation Various sedimentary structures Environment of formation History of... formation History of formation Rock Classification Review for Exam Reading the Grand Canyon The Grand Canyon Fig 8.16 The Grand Staircase 5 Coconino Sandstone 4 Redwall Limestone Sedimentary Rocks Intrusive Igneous Metamorphic 3 Bright Angel Shale 2 Grand Canyon Pink Granite 1 Vishnu Schist (and gneiss) The Grand Staircase Fig 8.16 Eastern Zion National Park Checkerboard Butte Zion National Park Vishnu