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The stishovite paradox in the evolution of lower mantle magmas and diamond-forming melts (experiment at 24 and 26 GPa).
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- Doklady Earth Sciences, 2017, v. 473, n. 2, p. 444, doi. 10.1134/S1028334X17040122
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- Article
Evolution of Diamond-Forming Systems of the Mantle Transition Zone: Ringwoodite Peritectic Reaction (Mg,Fe)<sub>2</sub>SiO<sub>4</sub> (Experiment at 20 GPa).
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- Geochemistry International, 2019, v. 57, n. 9, p. 1000, doi. 10.1134/S0016702919090118
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- Article