Partial Melting
Partial Melting is a magmatic process in which a polycrystalline rock undergoes incongruent melting such that only certain mineral phases melt at lower temperatures, producing a silicate melt compositionally distinct from the bulk rock while leaving a refractory residue.
9.8K
Publications
730.7K
Citations
18.2K
Authors
3K
Institutions
Publications per year
2017–2026
1.7K
9.8K
Size effect on the melting temperature of gold particles
Ph. Buffat, JP Borel · Physical review. A, General physics · 1976 · 3.3K citations · Full text
1–5 of 9.8K
18.2K
46
h-index
46
h-index
43
h-index
42
h-index
37
h-index
1–5 of 18.2K
3K

Centre National de la Recherche Scientifique
Paris, France
104 h-index
1.4K publications
100.6K citations

Australian National University
Canberra, Australia
79 h-index
332 publications
65K citations

Carnegie Institution for Science
Washington, United States
78 h-index
288 publications
31.2K citations

University of Bristol
Bristol, United Kingdom
77 h-index
299 publications
37.5K citations
California Institute of Technology
Pasadena, United States
76 h-index
308 publications
37.4K citations
ETH Zurich
Zurich, Switzerland
67 h-index
317 publications
29.8K citations
University of Bayreuth
Bayreuth, Germany
67 h-index
351 publications
28.7K citations
Planetary Science Institute
Tucson, United States
64 h-index
259 publications
25.3K citations
1–8 of 3K
518 publications · 49.1K citations
126
h-index
406 publications · 62.9K citations
126
h-index
438 publications · 48.6K citations
122
h-index
448 publications · 49.5K citations
117
h-index
JGR · 343 publications · 43K citations
116
h-index
1–5