Fault Breccia
Fault breccia is a type of fault rock characterized by angular clasts and fragmented particles formed through brittle deformation within a fault zone, distinguished from other fault rocks by its lack of significant mineral alignment and its genesis via mechanical shattering during seismic slip.
279
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798
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320
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2017–2026
46
279
Fault rocks and fault mechanisms
Richard H. Sibson · Journal of the Geological Society · 1977 · 2.1K citations
Hydraulic fracturing and mineralization
William J. Phillips · Journal of the Geological Society · 1972 · 363 citations
Classification of fault breccias and related fault rocks
Nigel Woodcock, Kate Mort · Geological Magazine · 2008 · 299 citations
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University of Cambridge
Cambridge, United Kingdom
11 h-index
26 publications
1.8K citations
Ruhr University Bochum
Bochum, Germany
11 h-index
19 publications
717 citations

Centre National de la Recherche Scientifique
Paris, France
9 h-index
22 publications
1.2K citations
Geological Survey of Canada
Ottawa, Canada
8 h-index
9 publications
296 citations

Durham University
Durham, United Kingdom
6 h-index
13 publications
619 citations
Niğde Ömer Halisdemir Üniversitesi
Niğde, Türkiye
6 h-index
12 publications
663 citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
6 h-index
16 publications
317 citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
5 h-index
10 publications
325 citations
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17 publications · 633 citations
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17 publications · 644 citations
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JGS · 13 publications · 2.9K citations
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JGR · 11 publications · 452 citations
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10 publications · 274 citations
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