Pyroxenite Geochemistry
Pyroxenite Geochemistry is a specialized branch of mantle geochemistry that investigates the composition, origin, and petrogenetic evolution of pyroxenites—mafic ultramafic rocks predominantly composed of pyroxene minerals—within the Earth's mantle, distinguishing itself by focusing on their distinct geochemical signatures, isotopic systematics, and roles in mantle heterogeneity and melt generation processes.
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2017–2026
119
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Yongsheng Liu, Shunbao Gao, Zhaoping Hu et al. · Journal of Petrology · 2009 · 3.7K citations
Othmar Müntener, P. B. Kelemen, T. L. Grove · Contributions to Mineralogy and Petrology · 2001 · 742 citations · Full text
Alkalic magmas generated by partial melting of garnet pyroxenite
M. M. Hirschmann, Tetsu Kogiso, Michael B. Baker et al. · Geology · 2003 · 546 citations
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Centre National de la Recherche Scientifique
Paris, France
29 h-index
132 publications
7.6K citations

Chinese Academy of Sciences
Beijing, China
27 h-index
163 publications
8.4K citations

Macquarie University
Sydney, Australia
22 h-index
87 publications
4.4K citations

University of the Witwatersrand
Johannesburg, South Africa
19 h-index
33 publications
2.4K citations
Institute of Geology and Geophysics
Beijing, China
19 h-index
66 publications
4.1K citations

China University of Geosciences (Beijing)
Beijing, China
17 h-index
57 publications
2.5K citations
China University of Geosciences
Wuhan, China
17 h-index
96 publications
25.9K citations
Guangzhou Institute of Geochemistry
Guangzhou, China
16 h-index
57 publications
3.4K citations
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97 publications · 11.9K citations
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