Subduction Zone Facies
Subduction Zone Facies is a metamorphic facies assemblage characterized by high-pressure, low-temperature mineral assemblages formed under the distinctive P-T conditions of subducting oceanic crust within a convergent plate boundary setting.
306
Publications
20.3K
Citations
966
Authors
387
Institutions
Publications per year
2017–2026
59
Parents
306
Intracontinental subduction: a possible mechanism for the Early Palaeozoic Orogen of SE China
Michel Faure, Liangshu Shu, Bo Wang et al. · Terra Nova · 2009 · 418 citations · Full text
1–5 of 306
966
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University of California, Santa Barbara, United States
5 publications · 1.3K citations
5
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1–5 of 966
387

Centre National de la Recherche Scientifique
Paris, France
18 h-index
47 publications
4.1K citations

Chinese Academy of Sciences
Beijing, China
16 h-index
36 publications
3.8K citations
Institute of Geology and Geophysics
Beijing, China
11 h-index
23 publications
3K citations
Stanford University
Stanford, United States
10 h-index
16 publications
1.1K citations
University of Bern
Bern, Switzerland
9 h-index
20 publications
2.1K citations
Curtin University
Perth, Australia
9 h-index
15 publications
1.3K citations
University of California, Santa Barbara
Santa Barbara, United States
9 h-index
18 publications
2K citations
China University of Geosciences
Wuhan, China
9 h-index
28 publications
1.4K citations
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35 publications · 2.8K citations
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18 publications · 1K citations
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15 publications · 1.4K citations
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14 publications · 1.3K citations
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JGS · 13 publications · 684 citations
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