Cataclasis
Cataclasis is a deformation mechanism characterized by the brittle fracturing and granulation of rock material under stress, distinguishing it from ductile or plastic deformation processes through the dominant role of microfracturing and grain size reduction.
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2017–2026
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Self-similar cataclasis in the formation of fault gouge
C. G. Sammis, Robert H. Osborne, J. Lawford Anderson et al. · Pure and Applied Geophysics · 1986 · 229 citations
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Centre National de la Recherche Scientifique
Paris, France
3 h-index
5 publications
488 citations

Durham University
Durham, United Kingdom
3 h-index
5 publications
429 citations

University of Otago
Dunedin, New Zealand
3 h-index
5 publications
166 citations

University of Liverpool
Liverpool, United Kingdom
2 h-index
4 publications
120 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
2 h-index
9 publications
616 citations

University of Louisville
Louisville, United States
2 h-index
3 publications
78 citations
Uni Research (Norway)
Bergen, Norway
2 h-index
4 publications
76 citations
Natural History Museum
London, United Kingdom
2 h-index
4 publications
46 citations
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9 publications · 375 citations
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7 publications · 343 citations
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JGR · 4 publications · 326 citations
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JGS · 3 publications · 258 citations
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