Uhp Metamorphism
UHP Metamorphism is a type of metamorphic process characterized by mineralogical transformations occurring at pressures exceeding 2.5–3.0 GPa, typically associated with subduction of continental crust to mantle depths, distinguishing it from other metamorphic facies by the preservation of high-pressure index minerals such as coesite or diamond.
325
Publications
20.8K
Citations
791
Authors
267
Institutions
Publications per year
2017–2026
41
Variants
Ultra-high Pressure Metamorphism
Parents
325
The fall and rise of metamorphic zircon
Matthew J. Kohn, S. L. Corrie, Christopher Markley · American Mineralogist · 2015 · 295 citations
1–5 of 325
791
22
h-index
16
h-index
12
h-index
12
h-index
12
h-index
1–5 of 791
267

Chinese Academy of Geological Sciences
Beijing, China
34 h-index
154 publications
12.8K citations
Stanford University
Stanford, United States
30 h-index
72 publications
7.1K citations

Chinese Academy of Sciences
Beijing, China
24 h-index
71 publications
4.3K citations
Institute of Geology and Geophysics
Beijing, China
22 h-index
69 publications
3.8K citations

Peking University
Beijing, China
22 h-index
67 publications
5K citations
University of Science and Technology of China
Hefei, China
21 h-index
81 publications
6.6K citations
China University of Geosciences
Wuhan, China
20 h-index
66 publications
3.4K citations
Czech Academy of Sciences, Institute of Geology
Prague, Czechia
15 h-index
37 publications
2.3K citations
1–8 of 267
42 publications · 3.3K citations
33
h-index
39 publications · 2.4K citations
25
h-index
21 publications · 1.8K citations
20
h-index
21 publications · 1.8K citations
20
h-index
16 publications · 806 citations
14
h-index
1–5