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11. Using the facies diagram below connect slope on a P-T plot (= geothermal gradient) to the different types of metamorphism AND to the tectonic settings where they form.

11. Using the facies diagram below connect slope on a P-T plot (= geothermal gradient) to the different types of metamorphism AND to the tectonic settings where they form.

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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11. Using the facies diagram below connect slope on a P-T plot (= geothermal gradient) to the different types of AND to the tectonic settings where they form. metamorphism P kbar 14 12 10 4 2 00 Not realized on Earth Pumpellyite Prehnite- Zeolite 200 Blueschist Model Geotherm Greenschist 400 Eclogite And T°C Epidote Amphibolite Sil 600 Amphibolite 30°C/km Granulite Granite minimum 800 (modified from Spear, 1993) 1000
Transcribed Image Text:11. Using the facies diagram below connect slope on a P-T plot (= geothermal gradient) to the different types of AND to the tectonic settings where they form. metamorphism P kbar 14 12 10 4 2 00 Not realized on Earth Pumpellyite Prehnite- Zeolite 200 Blueschist Model Geotherm Greenschist 400 Eclogite And T°C Epidote Amphibolite Sil 600 Amphibolite 30°C/km Granulite Granite minimum 800 (modified from Spear, 1993) 1000
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