Garnet Peridotite is a type of ultramafic, mantle-derived igneous rock that belongs to the peridotite class and is distinguished by the presence of garnet as a major mineral phase, typically formed at depths exceeding approximately 80 kilometers where pressure stabilizes garnet over spinel or plagioclase in the mineral assemblage.
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The Redox State of Earth's Mantle
D. J. Frost, Catherine McCammon · Annual Review of Earth and Planetary Sciences · 2008 · 1.1K citations
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Centre National de la Recherche Scientifique
Paris, France
27 h-index
72 publications
6K citations
Stanford University
Stanford, United States
23 h-index
58 publications
4.5K citations
Chinese Academy of Geological Sciences
Beijing, China
22 h-index
85 publications
6.2K citations
Australian National University
Canberra, Australia
18 h-index
33 publications
3.9K citations
China University of Geosciences
Wuhan, China
17 h-index
45 publications
2.5K citations
Chinese Academy of Sciences
Beijing, China
17 h-index
55 publications
2.3K citations
Université de Montpellier
Montpellier, France
15 h-index
31 publications
1.8K citations
Carnegie Institution for Science
Washington, United States
15 h-index
21 publications
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- Journal of Petrology
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- Contributions to Mineralogy and Petrology
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- Lithos
51 publications · 2.6K citations
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- Journal of Metamorphic Geology
43 publications · 3.3K citations
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- Earth and Planetary Science Letters
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