Microrelief of Rounded Diamond Crystals as an Indicator of the Redox Conditions of Their Resorption in a Kimberlite Melt

We conducted a detailed study of the morphology of diamond crystals partially dissolved in a water-bearing kimberlite melt at pressure of 6.3 GPa, temperature of 1400 &#176;C, and two oxygen fugacities (fO<sub>2</sub>) corresponding to the Re-ReO<sub>2</sub> buffer and ne...

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Bibliographic Details
Main Authors: Alexander F. Khokhryakov, Denis V. Nechaev, Alexander G. Sokol
Format: Article
Language:English
Published: MDPI AG 2020-03-01
Series:Crystals
Subjects:
Online Access:https://www.mdpi.com/2073-4352/10/3/233