Deuteric Alteration is a type of mineral alteration that occurs through the interaction of minerals with magmatic volatiles or residual hydrothermal fluids during the late stages of magma crystallization, distinguishing it from alteration processes driven by external meteoric or metamorphic fluids.
61
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3.7K
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153
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85
Institutions
Publications per year
2017–2026
4
Parents
Publications
61
1–5 of 61
Authors
153
- RH
6
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3
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3
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3
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3
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1–5 of 153
Institutions
85
Centre National de la Recherche Scientifique
Paris, France
5 h-index
12 publications
974 citations
University of Edinburgh
Edinburgh, United Kingdom
4 h-index
9 publications
831 citations
Lakehead University
Thunder Bay, Canada
4 h-index
5 publications
206 citations
Kumamoto University
Kumamoto, Japan
3 h-index
6 publications
166 citations
Geological Survey of Norway
Trondheim, Norway
2 h-index
3 publications
47 citations
Indian Institute of Technology Kharagpur
Kharagpur, India
2 h-index
3 publications
64 citations
Centre de Recherches Pétrographiques et Géochimiques
Vandœuvre-lès-Nancy, France
2 h-index
5 publications
419 citations
University of Cape Town
Rondebosch, South Africa
2 h-index
2 publications
65 citations
1–8 of 85
Venues
- Mineralogical Magazine
6 publications · 1.3K citations
6
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- Journal of Petrology
6 publications · 206 citations
6
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- Geophysical Journal International
GJI · 6 publications · 377 citations
6
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- Economic Geology
5 publications · 116 citations
5
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- Canadian Journal of Earth Sciences
4 publications · 89 citations
4
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1–5