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FAULT FAULT BRECCIA During faulting, rocks sliding past each other can be crushed forming what is called a fault breccia. How is a fault breccia different from a typical breccia? The clasts are too big to be classified as a breccia The fault breccia was made by tectonic rather than sedimentary processes. The clasts are not as angular as those of a regular breccia. The clasts are not made of sedimentary rock.

FAULT FAULT BRECCIA During faulting, rocks sliding past each other can be crushed forming what is called a fault breccia. How is a fault breccia different from a typical breccia? The clasts are too big to be classified as a breccia The fault breccia was made by tectonic rather than sedimentary processes. The clasts are not as angular as those of a regular breccia. The clasts are not made of sedimentary rock.

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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FAULT FAULT BRECCIA During faulting, rocks sliding past each other can be crushed forming what is called a fault breccia. How is a fault breccia different from a typical breccia? The clasts are too big to be classified as a breccia The fault breccia was made by tectonic rather than sedimentary processes. The clasts are not as angular as those of a regular breccia. The clasts are not made of sedimentary rock. All of the above.
Transcribed Image Text:FAULT FAULT BRECCIA During faulting, rocks sliding past each other can be crushed forming what is called a fault breccia. How is a fault breccia different from a typical breccia? The clasts are too big to be classified as a breccia The fault breccia was made by tectonic rather than sedimentary processes. The clasts are not as angular as those of a regular breccia. The clasts are not made of sedimentary rock. All of the above.
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