Indicate how we can deduce that the metamorphism in the figure is of the regional metamorphism type. State Phylite -Schist. Gneiss. Migmatite ~100 C ~200 °C ~300 °C ~400 °C -~500 °C Part of formerly subducting crust a

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
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Question
Indicate how we can deduce that the metamorphism in the
figure is of the regional metamorphism type.
State
Phylite
-Schist.
Gneiss.
Migmatite
~100 C
~200 °C
~300 °C
~400 °C
-~500 °C
Part of formerly
subducting crust
a
Transcribed Image Text:Indicate how we can deduce that the metamorphism in the figure is of the regional metamorphism type. State Phylite -Schist. Gneiss. Migmatite ~100 C ~200 °C ~300 °C ~400 °C -~500 °C Part of formerly subducting crust a
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