Ophiolite-type diamond and deep genesis of chromitite

Acta Geoscientica Sinica, Volume 34, Issue 6, 2013, Pages 643-653.

Cited by: 10|Bibtex|Views31|DOI:https://doi.org/10.3975/cagsb.2013.06.01
WOS SCOPUS

Abstract:

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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