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Physico-Chemical Conditions of Crystallization and Ore Potential of Granitoids from the Boundary Zone of the Southern and Middle Urals
Snachev A., Snachev V., Znamensky S.
Manifestation of nitrogen interstitials in synthetic diamonds obtained using a temperature gradient technique (Fe–Ni–C system)
Babich Y., Feigelson B., Chepurov A.
Experimental Modeling of Formation of Native Metals (Fe, Ni, Co) in the Earth’s Crust by the Interaction of Hydrogen with Basaltic Melts
Persikov E., Bukhtiyarov P., Aranovich L., Nekrasov A., Shaposhnikova O.
Effect of sulfur concentration on diamond crystallization in the Fe–C–S system at 5.3–5.5 GPa and 1300–1370°C
Zhimulev E., Sonin V., Mironov A., Chepurov A.
Formation of Iron Hydride and Iron Carbide from Hydrocarbon Systems at Ultra-High Thermobaric Conditions
Serovaiskii A., Kolesnikov A., Kutcherov V.
Effect of Thermal State on the Mantle Composition and Core Sizes of the Moon
Kuskov O., Kronrod E., Kronrod V.
Experimental Study of Unequilibrated Silica Transfer from Liquid Water to the Vapor Phase
Alekseyev V., Medvedeva L., Balashov V., Burmistrov A., Gromyak I.
Silica Distribution in the System Quartz–Water–Vapor Depending on the Temperature Gradient
Alekseyev V., Medvedeva L.
Viscosity of Depolymerized Dunite Melts under Medium and High Pressures
Persikov E., Bukhtiyarov P., Sokol A.
Crystallization temperature of anatectic melt: An example of biotite–muscovite granite in the Rikolatvi structure, Belomorian Mobile Belt
Shcherbakova T.
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