Ultramafic Rocks
Ultramafic Rocks is an igneous rock type distinguished by a composition containing less than 45% silica and predominantly composed of mafic minerals such as olivine and pyroxene, with a high magnesium and iron content.
3.2K
Publications
173.4K
Citations
7.8K
Authors
1.7K
Institutions
Publications per year
2017–2026
569
Parents
3.2K
1–5 of 3.2K
7.8K
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Centre National de la Recherche Scientifique
Paris, France
55 h-index
435 publications
32.5K citations

Chinese Academy of Sciences
Beijing, China
51 h-index
389 publications
23.3K citations
United States Geological Survey
Reston, United States
39 h-index
172 publications
9.8K citations
Stanford University
Stanford, United States
38 h-index
105 publications
13.4K citations

Chinese Academy of Geological Sciences
Beijing, China
38 h-index
211 publications
15.5K citations

China University of Geosciences (Beijing)
Beijing, China
37 h-index
164 publications
12.1K citations

Australian National University
Canberra, Australia
35 h-index
71 publications
4.8K citations
Institute of Geology and Geophysics
Beijing, China
32 h-index
192 publications
11.4K citations
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153 publications · 14.5K citations
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149 publications · 8.2K citations
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109 publications · 6.9K citations
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82 publications · 4.8K citations
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JGR · 68 publications · 7.5K citations
41
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