Cataclastic Deformation is a brittle deformation process characterized by the granulation, crushing, and frictional sliding of rock fragments within fault zones, resulting from mechanical breakdown and grain-size reduction under sub-greenschist facies conditions.
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Cataclasis and the Generation of Fault Gouge
J. T. Engelder · Geological Society of America Bulletin · 1974 · 442 citations
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Centre National de la Recherche Scientifique
Paris, France
17 h-index
37 publications
2.4K citations
Stony Brook University
Stony Brook, United States
13 h-index
27 publications
4.3K citations
Université de Strasbourg
Strasbourg, France
11 h-index
18 publications
1.8K citations
State University of New York
Albany, United States
10 h-index
19 publications
2.4K citations
University of Bergen
Bergen, Norway
7 h-index
27 publications
1.8K citations
University of Liverpool
Liverpool, United Kingdom
6 h-index
12 publications
445 citations
University of Vienna
Vienna, Austria
6 h-index
17 publications
672 citations
Institut de physique du globe de Paris
Paris, France
6 h-index
8 publications
812 citations
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- Journal of Geophysical Research Atmospheres
JGR · 34 publications · 5.4K citations
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- Journal of Structural Geology
34 publications · 2.1K citations
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- Geological Society London Special Publications
13 publications · 645 citations
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- Tectonophysics
14 publications · 657 citations
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- Journal of Geophysical Research Solid Earth
12 publications · 548 citations
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