MgCO3 + SiO2 Reaction at Pressures up to 32 GPa Studied Using in-Situ X-Ray Diffraction and Synchrotron Radiation › Research Explorer

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MgCO₃ + SiO₂ Reaction at Pressures up to 32 GPa Studied Using in-Situ X-Ray Diffraction and Synchrotron Radiation

Research output: Contribution to journal › Article › peer-review

Laboratory for Experimental Geochemistry and Petrology of the Earth's Mantle

DOI

https://doi.org/10.1134/S0016702919090064
Final published version

K. D. Litasov
A. F. Shatskiy

Original language	English
Pages (from-to)	1024-1033
Number of pages	10
Journal	Geochemistry International
Volume	57
Issue number	9
DOIs	https://doi.org/10.1134/S0016702919090064
Publication status	Published - 1 Sept 2019

OECD FOS+WOS

Research areas

bridgmanite, carbonate, coesite, enstatite, magnesite, mantle, melting, stishovite, transition zone, 32 GPA, SYSTEM, HIGH-PRESSURE, CARBONATED ECLOGITE, HIGH-TEMPERATURE, PERIDOTITE, LOWER MANTLE, DIAMOND FORMATION, MAGNESITE, PHASE-RELATIONS

ID: 21344191