Felsic Magmatism
Felsic Magmatism is a type of magmatic process characterized by the generation, ascent, and emplacement of silica-rich, typically granitic to rhyolitic magmas derived from partial melting of crustal or upper mantle sources under specific thermal and tectonic conditions.
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Two contrasting granite types: 25 years later
B. W. Chappell, A. J. R. White · Australian Journal of Earth Sciences · 2001 · 1.5K citations
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Centre National de la Recherche Scientifique
Paris, France
35 h-index
120 publications
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Chinese Academy of Sciences
Beijing, China
33 h-index
184 publications
13.6K citations

Australian National University
Canberra, Australia
32 h-index
74 publications
8.1K citations

China University of Geosciences (Beijing)
Beijing, China
30 h-index
140 publications
11.8K citations
Institute of Geology and Geophysics
Beijing, China
24 h-index
60 publications
5.2K citations

Chinese Academy of Geological Sciences
Beijing, China
24 h-index
102 publications
5.6K citations

Monash University
Melbourne, Australia
20 h-index
42 publications
2.9K citations

The University of Adelaide
Adelaide, Australia
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40 publications
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JGS · 40 publications · 3.4K citations
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