Hydrous Magmatism
Hydrous Magmatism is a type of magmatic process occurring in plutonic environments characterized by the significant presence and influence of water-rich fluids on magma generation, evolution, and crystallization.
628
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58.4K
Citations
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588
Institutions
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2017–2026
148
Parents
628
Bradley R. Hacker, Simon M. Peacock, G. A. Abers et al. · Journal of Geophysical Research Atmospheres · 2003 · 1K citations · Full text
Water in Earth's Mantle: The Role of Nominally Anhydrous Minerals
David Bell, George R. Rossman · Science · 1992 · 954 citations
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Centre National de la Recherche Scientifique
Paris, France
32 h-index
137 publications
8.2K citations
University of Bayreuth
Bayreuth, Germany
23 h-index
56 publications
5.7K citations

Carnegie Institution for Science
Washington, United States
21 h-index
42 publications
5.9K citations

Chinese Academy of Sciences
Beijing, China
20 h-index
96 publications
5.2K citations
Planetary Science Institute
Tucson, United States
19 h-index
43 publications
6K citations
ETH Zurich
Zurich, Switzerland
19 h-index
37 publications
3.5K citations

Tohoku University
Sendai, Japan
19 h-index
53 publications
5.6K citations
California Institute of Technology
Pasadena, United States
17 h-index
36 publications
6.3K citations
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