Physics
Scientist
Institute of Experimental Mineralogy, Russian Academy of Sciences
Magmatic Transport of Carbon, Hydrogen and Nitrogen Constituents from Reduced Planetary Interiors
Mantle carbonatite magma in diamond genesis
Mantle genesis of diamond in carbonate-silicate-carbon melts of variable chemistry: Evidence from high-pressure experiments
New synthetic high-density nickel sulfide: A plausible component of the Earth's core and terrestrial planets
The Role of Hydrogen and Oxygen Fugacity on the Incorporation of Nitrogen in Reduced Magmas of the Early Earth's Mantle
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