The presence of migmatites in an area is indicative of deep-seated fault-zone metamorphism. A Fault breccia B) Cataclasite True D) Mylonite Batholiths and stocks are examples of concordant intrusive bodies. A) Discordant B) Tabular Massive D) True
The presence of migmatites in an area is indicative of deep-seated fault-zone metamorphism. A Fault breccia B) Cataclasite True D) Mylonite Batholiths and stocks are examples of concordant intrusive bodies. A) Discordant B) Tabular Massive D) True
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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![The presence of migmatites in an area is indicative of deep-seated fault-zone metamorphism.
A) Fault breccia
B) Cataclasite
C) True
D) Mylonite
Batholiths and stocks are examples of concordant intrusive bodies.
A) Discordant
B) Tabular
C) Massive
D) True](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F01bd01be-adf9-4388-b434-e34bea90f8ae%2F745429de-f2b1-4599-a948-cabcb875d30c%2Fv8j3c2n_processed.png&w=3840&q=75)
Transcribed Image Text:The presence of migmatites in an area is indicative of deep-seated fault-zone metamorphism.
A) Fault breccia
B) Cataclasite
C) True
D) Mylonite
Batholiths and stocks are examples of concordant intrusive bodies.
A) Discordant
B) Tabular
C) Massive
D) True
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