Hp Metamorphism
HP Metamorphism is a type of regional metamorphism characterized by high-pressure and relatively low-temperature conditions, typically occurring in subduction zones, that results in the formation of distinctive mineral assemblages diagnostic of such pressure-temperature regimes.
170
Publications
9.9K
Citations
556
Authors
235
Institutions
Publications per year
2017–2026
30
Parents
170
1–5 of 170
556
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Laboratoire de Géologie de l’École Normale Supérieure, France
4 publications · 440 citations
4
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4
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University of California, Santa Barbara, United States
4 publications · 311 citations
4
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1–5 of 556
235

Centre National de la Recherche Scientifique
Paris, France
21 h-index
58 publications
5.1K citations

Chinese Academy of Geological Sciences
Beijing, China
17 h-index
43 publications
2.6K citations

Chinese Academy of Sciences
Beijing, China
14 h-index
48 publications
2.8K citations
Institute of Geology and Geophysics
Beijing, China
12 h-index
42 publications
2.1K citations

Peking University
Beijing, China
10 h-index
32 publications
1.3K citations
China University of Geosciences
Wuhan, China
7 h-index
24 publications
1.8K citations
University of Lausanne
Lausanne, Switzerland
7 h-index
15 publications
619 citations
University of California, Santa Barbara
Santa Barbara, United States
6 h-index
12 publications
889 citations
1–8 of 235
27 publications · 1.8K citations
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14 publications · 721 citations
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12 publications · 451 citations
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8 publications · 592 citations
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7 publications · 464 citations
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