Chapter 21: Metamorphism - Faculty web pages

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$Math 361 Problem Set #5 Due 5 October 2012 - Faculty web pages$

$Math 362 Problem Set #9 â€“ Solution 27 April 2012 - Faculty web ...$

The Types of MetamorphismDifferent approaches to classification2. Based on setting Contact Metamorphism Regional MetamorphismOrogenic MetamorphismBurial MetamorphismOcean Floor Metamorphism Shock Metamorphism
Contact Metamorphism• Adjacent to igneous intrusions• Result of thermal (and possibly metasomatic)effects of hot magma intruding cooler shallowrocks• Occur over a wide range of pressures, includingvery low• Contact aureole
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: The Types of MetamorphismDifferent
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 and 40: To summarize:• An isograd represe
Page 41 and 42: Paired Metamorphic Belts of Japan
Page 43 and 44: Figure 21-12. The Sanbagawa andRyok
Page 45 and 46: Paired Metamorphic Belts of Japan

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