Trace Element Fractionation
Trace Element Fractionation is a geochemical process characterized by the preferential partitioning of trace elements between coexisting phases during magmatic crystallization, metamorphic reactions, or weathering transformations, driven by differences in ionic radius, valence state, and site occupancy that distinguish it from major element behavior.
243
Publications
34.2K
Citations
764
Authors
338
Institutions
Publications per year
2017–2026
30
243
Trace element fractionation during anatexis
Denis M. Shaw · Geochimica et Cosmochimica Acta · 1970 · 2K citations
1–5 of 243
764
5
h-index
4
h-index
4
h-index
4
h-index
3
h-index
1–5 of 764
338

Centre National de la Recherche Scientifique
Paris, France
17 h-index
47 publications
5.3K citations
University of Chicago
Chicago, United States
11 h-index
18 publications
1.7K citations
University of California, Los Angeles
Los Angeles, United States
10 h-index
15 publications
4.4K citations
Planetary Science Institute
Tucson, United States
10 h-index
15 publications
1.5K citations

Chinese Academy of Sciences
Beijing, China
8 h-index
29 publications
1.3K citations

Australian National University
Canberra, Australia
7 h-index
14 publications
8.2K citations

Macquarie University
Sydney, Australia
7 h-index
14 publications
1.5K citations

University of Bristol
Bristol, United Kingdom
7 h-index
16 publications
2.4K citations
1–8 of 338
44 publications · 7.7K citations
33
h-index
17 publications · 1.7K citations
17
h-index
16 publications · 10K citations
16
h-index
15 publications · 2.9K citations
15
h-index
15 publications · 2.2K citations
15
h-index
1–5