Intermediate Magmatism
Intermediate Magmatism is a type of magmatic differentiation process characterized by the generation, evolution, and emplacement of magmas with intermediate silica content (typically 52–63 wt% SiO₂), distinguising it from mafic and felsic magmatism through its distinct petrogenetic pathways, mineralogical assemblages, and tectonic settings.
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7.8K
Citations
419
Authors
218
Institutions
Publications per year
2017–2026
31
Parents
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1–5 of 120
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University of North Carolina at Chapel Hill, United States
3 publications · 265 citations
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2
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2
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1–5 of 419
218

Chinese Academy of Sciences
Beijing, China
7 h-index
24 publications
1.5K citations

Macquarie University
Sydney, Australia
6 h-index
8 publications
598 citations
Institute of Geology and Geophysics
Beijing, China
5 h-index
13 publications
711 citations
ETH Zurich
Zurich, Switzerland
4 h-index
10 publications
1.1K citations

Durham University
Durham, United Kingdom
4 h-index
5 publications
267 citations
China University of Geosciences
Wuhan, China
4 h-index
15 publications
280 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
9 publications
860 citations

China University of Geosciences (Beijing)
Beijing, China
4 h-index
11 publications
289 citations
1–8 of 218
10 publications · 583 citations
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10 publications · 656 citations
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JGR · 6 publications · 986 citations
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6 publications · 425 citations
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5 publications · 736 citations
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