Ht Metamorphism
HT Metamorphism is a type of regional metamorphism characterized by high temperature relative to pressure, typically associated with deep crustal conditions and the development of metamorphic facies such as granulite and amphibolite, distinguishing it from low-temperature or high-pressure metamorphic regimes.
57
Publications
3.5K
Citations
223
Authors
125
Institutions
Publications per year
2017–2026
9
Variants
High-temperature Metamorphism
Parents
57
Rebecca A. Jamieson, Christopher Beaumont, Sergei Medvedev et al. · Journal of Geophysical Research Atmospheres · 2004 · 420 citations · Full text
Vojtĕch Janoušek, František V. Holub · Proceedings of the Geologists Association · 2007 · 173 citations
Fritz Finger, Axel Gerdes, Vojtĕch Janoušek et al. · Journal of Geosciences · 2007 · 158 citations · Full text
1–5 of 57
223
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4
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3
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3
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3
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125

Centre National de la Recherche Scientifique
Paris, France
9 h-index
33 publications
1.7K citations
Charles University
Prague, Czechia
4 h-index
9 publications
367 citations
Géosciences Rennes
Rennes, France
4 h-index
10 publications
759 citations
Bureau de Recherches Géologiques et Minières
Orléans, France
4 h-index
4 publications
206 citations
ETH Zurich
Zurich, Switzerland
4 h-index
7 publications
587 citations

Université de Montpellier
Montpellier, France
4 h-index
7 publications
132 citations
Total (France)
Paris, France
3 h-index
7 publications
418 citations
Géosciences Montpellier
Montpellier, France
3 h-index
6 publications
122 citations
1–8 of 125
6 publications · 342 citations
6
h-index
JGS · 5 publications · 402 citations
5
h-index
4 publications · 267 citations
4
h-index
4 publications · 92 citations
4
h-index
3 publications · 66 citations
3
h-index
1–5