Tectonic Cleavage
Tectonic Cleavage is a geological structure, specifically a planar fabric formed within rocks due to the alignment of mineral grains or the development of submicroscopic foliation under directed pressure during regional metamorphism and deformation, distinguishing it from primary sedimentary layering or other non-tectonically induced anisotropies.
148
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8.7K
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425
Authors
219
Institutions
Publications per year
2017–2026
13
Parents
148
Geodynamic settings and tectonic model of skarn gold deposits in China: An overview
Yanjing Chen, Khin Zaw, Franco Pirajno et al. · Ore Geology Reviews · 2006 · 261 citations · Full text
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Chinese Academy of Sciences
Beijing, China
7 h-index
21 publications
1.2K citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
6 publications
336 citations

British Geological Survey
Nottingham, United Kingdom
4 h-index
7 publications
289 citations
KU Leuven
Leuven, Belgium
3 h-index
5 publications
155 citations
Institute of Geology and Geophysics
Beijing, China
3 h-index
8 publications
300 citations
United States Geological Survey
Reston, United States
3 h-index
5 publications
66 citations
Geological Survey of Canada
Ottawa, Canada
3 h-index
5 publications
138 citations

University of Hong Kong
Pok Fu Lam, Hong Kong
3 h-index
8 publications
725 citations
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15 publications · 1.6K citations
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9 publications · 314 citations
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9 publications · 633 citations
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8 publications · 282 citations
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6 publications · 287 citations
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