Chapter 21: Metamorphism - Faculty web pages

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Paired Metamorphic Belts of JapanFigure <strong>21</strong>-12. The Sanbagawa andRyoke metamorphic belts of Japan.From Turner (1981) MetamorphicPetrology: Mineralogical, Field, andTectonic Aspects. McGraw-Hill andMiyashiro (1994) Metamorphic Petrology.Oxford University Press.
Paired Metamorphic Belts of Japan• The “inner” belt, inward, or away from the trench isthe Ryoke -AbukumaBeltLow P/T regional orogenic metamorphismDominant meta-pelitic sediments, and isograds up to thesillimanite zone have been mappedA high-temperaturetemperature-low-pressurebelt, and graniticplutons are common
Page 2: The Limits of Metamorphism• Low-t
Page 5 and 6: Metamorphic Agents and ChangesIncre
Page 7 and 8: Figure 21-1. Metamorphic field grad
Page 9 and 10: Stress• Lithostatic pressure is u
Page 11 and 12: •Deviatoricstress affects the tex
Page 13 and 14: Fluids• P fluid indicates the tot
Page 15 and 16: The Types of MetamorphismDifferent
Page 17 and 18: Contact Metamorphism• Adjacent to
Page 19 and 20: The Types of MetamorphismContact Me
Page 21 and 22: The Types of MetamorphismOrogenic M
Page 23 and 24: The Types of MetamorphismOrogenic M
Page 25 and 26: The Types of MetamorphismBurial met
Page 27 and 28: The Types of MetamorphismOcean-Floo
Page 29 and 30: The Progressive Nature of Metamorph
Page 31 and 32: Each rock preserves the conditions
Page 33 and 34: Types of ProtolithCommon types of s
Page 35 and 36: Orogenic Regional Metamorphism ofth
Page 37 and 38: The sequence of zones now recognize
Page 39: To summarize:• An isograd represe
Page 43 and 44: Figure 21-12. The Sanbagawa andRyok
Page 45 and 46: Paired Metamorphic Belts of Japan

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