High-pressure Metamorphism
High-Pressure Metamorphism is a type of metamorphic process characterized by mineralogical and chemical transformations occurring under unusually elevated pressure conditions, typically associated with subduction zones or continental collision settings, where the dominant variable distinguishing it from other metamorphic pathways is the exceptionally high pressure relative to temperature.
784
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1.8K
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593
Institutions
Publications per year
2017–2026
99
784
Evolution of Metamorphic Belts
Akiho Miyashiro · Journal of Petrology · 1961 · 1.2K citations
Diamond from the Dabie Shan Metamorphic Rocks and Its Implication for Tectonic Setting
Shutong Xu, Su Wen, Shouyuan Ji et al. · Science · 1992 · 837 citations
Keqing Zong, Reiner Klemd, Yu Yuan et al. · Precambrian Research · 2016 · 742 citations
Urs Schaltegger, C. Mark Fanning, Detlef Günther et al. · Contributions to Mineralogy and Petrology · 1999 · 683 citations
Yongsheng Liu, Keqing Zong, P. B. Kelemen et al. · Chemical Geology · 2007 · 603 citations
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Laboratoire de Géologie de l’École Normale Supérieure, France
11 publications · 1.2K citations
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Centre National de la Recherche Scientifique
Paris, France
31 h-index
116 publications
13.1K citations

Chinese Academy of Geological Sciences
Beijing, China
24 h-index
60 publications
6.1K citations

Australian National University
Canberra, Australia
23 h-index
37 publications
4.2K citations

Chinese Academy of Sciences
Beijing, China
22 h-index
81 publications
6.2K citations
Ruhr University Bochum
Bochum, Germany
22 h-index
49 publications
4.2K citations
Institute of Geology and Geophysics
Beijing, China
20 h-index
66 publications
5.5K citations
Stanford University
Stanford, United States
16 h-index
37 publications
4.1K citations

Peking University
Beijing, China
16 h-index
40 publications
2.8K citations
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46 publications · 4.5K citations
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42 publications · 2.9K citations
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37 publications · 1.9K citations
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