The Peritectic Reaction of Olivine as the Mechanism of the Ultrabasic–Basic Evolution of the Diamond-Forming Silicate-Carbonate-(C-O-H) System: Experiments at 6.0 GPa

The Peritectic Reaction of Olivine as the Mechanism of the Ultrabasic–Basic Evolution of the Diamond-Forming Silicate-Carbonate-(C-O-H) System: Experiments at 6.0 GPa

Melting phase relations of the diamond-forming olivine (Ol)–jadeite (Jd)–diopside (Di)–(Mg, Fe, Ca, Na)-carbonates (Carb)–(C-O-H-fluid) system are studied in experiments at 6.0 GPa in the polythermal Ol<sub>74</sub>Carb<sub>18.5</sub>(C-O-H)<sub>7.5</sub>-Omp<s...

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Bibliographic Details
Main Authors: Yuriy A. Litvin, Anastasiya V. Kuzyura, Anna V. Spivak
Format: Article
Language:English
Published: MDPI AG 2023-08-01
Series:Minerals
Subjects:
diamond-forming silicate-carbonate system
C-O-H fluid
peritectic reaction of olivine
ultrabasic–basic evolution
origin of diamond-bearing peridotites and eclogites
high pressure and temperature
Online Access:https://www.mdpi.com/2075-163X/13/8/1040

Internet

https://www.mdpi.com/2075-163X/13/8/1040

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