Chapter 8: Major Elements - Faculty web pages

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

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Fig. 26-19. Simplified petrogenetic grid for metamorphosed mafic rocks showing the location of several determined univariant reactions in the CaO-MgO MgO-Al 2 O 3 -SiO 2 -H 2 O-(Na 2 O) system (“C(N)MASH( C(N)MASH”). ). Winter (2001) An Introduction to Igneous and Metamorphic Petrology. Prentice Hall.
Greenschist, Amphibolite, Granulite Facies The granulite facies is characterized by the presence of a largely anhydrous mineral assemblage Metabasites critical mineral assemblage is orthopyroxene + clinopyroxene + plagioclase + quartz Garnet, minor hornblende and/or biotite may be present Fig. 25-8. ACF diagram for the granulite facies. The composition range of common mafic rocks is shaded. Winter (2001) An Introduction to Igneous and Metamorphic Petrology. Prentice Hall.
Page 1 and 2: Metamorphic Facies Eskola (1915) ,
Page 3 and 4: Metamorphic Facies Interpretive: :
Page 5 and 6: Metamorphic Facies In his final ac
Page 7 and 8: Metamorphic Facies Fig. 25-2. 2. Te
Page 9 and 10: It is convenient to consider metamo
Page 11 and 12: Fig. 25-2. 2. Temperature- pressure
Page 15 and 16: Metamorphic Facies Combine the conc
Page 17 and 18: Figure 21-1. Metamorphic field grad
Page 19 and 20: Facies Series High P/T series - occ
Page 21 and 22: Metamorphism of Mafic Rocks Most
Page 23 and 24: Metamorphism of Mafic Rocks Clin
Page 25 and 26: Mafic Assemblages of the Medium P/T
Page 27 and 28: Greenschist Facies Greenschist, A
Page 29 and 30: Amphibolite facies Greenschist
Page 31: Transition to Granulite Facies Maf
Page 35 and 36: Greenschist, Amphibolite, Granulite
Page 39 and 40: Mafic Assemblages of the High P/T S
Page 41 and 42: Blueschist and Eclogite Facies The
Page 43 and 44: Blueschist and Eclogite Facies Eclo
Page 45 and 46: Pressure-Temperature Temperature-Ti
Page 49 and 50: Fig. 25-13a. Conventional P-T P T d
Page 53 and 54: Fig. 25-12a. Schematic pressure-tem
Page 55 and 56: Fig. 25-12b. Schematic pressure-tem
Page 59 and 60: 2. P max and T max do not occur at
Page 61 and 62: This occurs at a pressure well belo
Page 63: Metamorphic field gradient - PT cha

Chapter 8: Major Elements - Faculty web pages

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