Ophiolite-type diamond and deep genesis of chromitite
Acta Geoscientica Sinica, Volume 34, Issue 6, 2013, Pages 643-653.
The three main occurrences of natural diamond currently recognized on Earth are kimberlites from the deep mantle under cratonic lithosphere, ultrahigh-pressure metamorphic rocks formed by subduction of continental crust, and meteorites and rocks in impact structures. Based on the discovery of diamonds and other ultrahigh-pressure minerals...More
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