Cuboctahedral type Ib diamonds in ophiolitic chromitites and peridotites: the evidence for anthropogenic contamination
Author:
Affiliation:
1. Sobolev Institute of Geology and Mineralogy, SB RAS, Novosibirsk, Russia
2. Department of Geology and Geophysics, Novosibirsk State University, Novosibirsk, Russia
3. Geochemical Research Center, University of Tokyo, Tokyo, Japan
Funder
Japan Society for Promotion of Science
Publisher
Informa UK Limited
Subject
Condensed Matter Physics
Link
https://www.tandfonline.com/doi/pdf/10.1080/08957959.2019.1616183
Reference33 articles.
1. Diamonds in ophiolites: Contamination or a new diamond growth environment?
2. Carbon and nitrogen isotope, and mineral inclusion studies on the diamonds from the Pozanti–Karsanti chromitite, Turkey
3. Ultra-high pressure minerals in the Luobusa Ophiolite, Tibet, and their tectonic implications
4. Origin of ultrahigh pressure and highly reduced minerals in podiform chromitites and associated mantle peridotites of the Luobusa ophiolite, Tibet
5. Diamonds, native elements and metal alloys from chromitites of the Ray-Iz ophiolite of the Polar Urals
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