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Experimental Study of the Multicomponent Chemical Diffusion of Major Components (SiO<sub>2,</sub> Al<sub>2</sub>O<sub>3,</sub> Na<sub>2</sub>O, CaO, MgO, and FeO) and the Anion at Interaction between Basalt and Kimberlite Melts under a Moderate Pressure.
- Published in:
- Petrology, 2022, v. 30, n. 3, p. 325, doi. 10.1134/S0869591122020060
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- Article
Interaction of Fe<sub>3</sub>C with Hydrogen: On the Compatibility of Carbon with Hydrogen in Metallic Iron.
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- Petrology, 2021, v. 29, n. 6, p. 695, doi. 10.1134/S0869591121060072
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- Article
Viscosity of Depolymerized Dunite Melts under Medium and High Pressures.
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- Geochemistry International, 2018, v. 56, n. 12, p. 1148, doi. 10.1134/S0016702918120078
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- Article
Gold Dissolution in Dry Salt Melts in the Presence of SiO<sub>2</sub> as a Function of P(O<sub>2</sub>).
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- Geochemistry International, 2018, v. 56, n. 3, p. 240, doi. 10.1134/S0016702918030084
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- Article
Gold transport during magmatic degassing: Model experiments.
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- Geochemistry International, 2016, v. 54, n. 11, p. 979, doi. 10.1134/S0016702916090093
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- Article
Eocene accretion at Kamchatka and a pulse of mantle plume magmatism.
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- Geochemistry International, 2015, v. 53, n. 4, p. 341, doi. 10.1134/S001670291502007X
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- Article
Concentration dependence of water diffusion in obsidian and dacitic melts at high-pressures.
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- Geochemistry International, 2014, v. 52, n. 5, p. 365, doi. 10.1134/S0016702914050085
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- Article
Erratum to: Some Features of the Process of Interaction of Iron with Methane at a Temperature of 900°C and a Pressure of 100 MPa.
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- 2024
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- Correction Notice
Some Features of the Process of Interaction of Iron with Methane at a Temperature of 900°C and a Pressure of 100 MPa.
- Published in:
- Doklady Earth Sciences, 2023, v. 512, n. 1, p. 819, doi. 10.1134/S1028334X2360113X
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- Article
Andesite Melt Crystallization under Moderate Hydrogen Pressures: An Experimental Study.
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- Geochemistry International, 2024, v. 62, n. 4, p. 366, doi. 10.1134/S0016702923700131
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- Article
Experimental Modeling of Formation of Native Metals (Fe, Ni, Co) in the Earth's Crust by the Interaction of Hydrogen with Basaltic Melts.
- Published in:
- Geochemistry International, 2019, v. 57, n. 10, p. 1035, doi. 10.1134/S0016702919100082
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- Publication type:
- Article