Magma Assimilation
Magma Assimilation is a geological process in which a magma absorbs and incorporates surrounding country rock through thermal or chemical interaction, thereby modifying its composition while crystallizing or ascending through the crust.
102
Publications
6.8K
Citations
285
Authors
162
Institutions
Publications per year
2017–2026
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162

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
5 h-index
13 publications
1.1K citations
United States Geological Survey
Reston, United States
5 h-index
6 publications
314 citations
California Institute of Technology
Pasadena, United States
4 h-index
7 publications
732 citations

Central Washington University
Ellensburg, United States
4 h-index
5 publications
271 citations

University of British Columbia
Vancouver, Canada
4 h-index
5 publications
307 citations
University of California, Santa Barbara
Santa Barbara, United States
4 h-index
6 publications
333 citations

Centre National de la Recherche Scientifique
Paris, France
4 h-index
6 publications
575 citations

Australian National University
Canberra, Australia
3 h-index
5 publications
275 citations
1–8 of 162
23 publications · 1.9K citations
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12 publications · 535 citations
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11 publications · 799 citations
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8 publications · 935 citations
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6 publications · 287 citations
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1–5