Why are diamonds preserved in UHP metamorphic complexes? Experimental evidence for the effect of pressure on diamond graphitization
Author:
Affiliation:
1. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia
2. Earth & Climate Sciences, San Francisco State University, San Francisco, CA, USA
Funder
Russian Science Foundation
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206814.2018.1435310
Reference114 articles.
1. Diamond dissolution rates in kimberlitic melts at 13001500 C in the graphite stability field
2. Geothermobarometric history of subduction recorded by quartz inclusions in garnet
3. Eclogites of the Snowbird tectonic zone: petrological and U-Pb geochronological evidence for Paleoproterozoic high-pressure metamorphism in the western Canadian Shield
4. Pliocene eclogite exhumation at plate tectonic rates in eastern Papua New Guinea
5. Using strain birefringence in diamond to estimate the remnant pressure on an inclusion
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