High-temperature Element Mobility
High-Temperature Element Mobility is a geochemical process that describes the relative ease and mechanisms by which chemical elements migrate and redistribute in silicate melts, magmatic fluids, and high-grade metamorphic systems under elevated temperature and pressure conditions typical of Earth’s crust and mantle, distinguished from low-temperature mobility processes by the dominant role of thermal energy, ionic diffusion, and phase equilibria in facilitating elemental transport.
11
Publications
749
Citations
44
Authors
24
Institutions
Publications per year
2017–2026
0
11
1–5 of 11
44
2
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24
University of California, Los Angeles
Los Angeles, United States
2 h-index
4 publications
524 citations

University of Hawaiʻi at Mānoa
Honolulu, United States
1 h-index
4 publications
108 citations

University of Windsor
Windsor, Canada
1 h-index
3 publications
102 citations

Sorbonne Université
Paris, France
1 h-index
1 publications
21 citations

Centre National de la Recherche Scientifique
Paris, France
1 h-index
4 publications
84 citations

University of Saskatchewan
Saskatoon, Canada
1 h-index
1 publications
34 citations

Monash University
Melbourne, Australia
1 h-index
1 publications
27 citations
Memorial University of Newfoundland
St. John's, Canada
1 h-index
3 publications
141 citations
1–8 of 24
4 publications · 512 citations
4
h-index
2 publications · 48 citations
2
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1 publications · 23 citations
1
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1 publications · 74 citations
1
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1 publications · 34 citations
1
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1–5