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Calculational study of the enrichment of cadmium isotopes in gas centrifuges.
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- Theoretical Foundations of Chemical Engineering, 2007, v. 41, n. 6, p. 851, doi. 10.1134/S0040579507060103
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- Article
Variability of Stishovite Genesis under Terrestrial Conditions: Physicogeochemical Aspects.
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- Geochemistry International, 2024, v. 62, n. 2, p. 124, doi. 10.1134/S0016702924020071
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Peritectic Reaction of Olivine in the Carbonate–Silicate–(C–O–H) Diamond-Forming System at 6 GPa.
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- Geochemistry International, 2024, v. 62, n. 1, p. 32, doi. 10.1134/S001670292401004X
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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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The system ilmenite-carbonatite-carbon in the origin of diamond: Correlation between the titanium content and diamond potential of kimberlite.
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- Doklady Earth Sciences, 2017, v. 473, n. 1, p. 286, doi. 10.1134/S1028334X17030059
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- Article
The system MgCO-FeCO-CaCO-NaCO at 12-23 GPa: Phase relations and significance for the genesis of ultradeep diamonds.
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- Doklady Earth Sciences, 2015, v. 464, n. 1, p. 946, doi. 10.1134/S1028334X15090135
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Partitioning of rare elements between diamond-forming melts and minerals of the peridotite-carbonatite system.
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- Doklady Earth Sciences, 2014, v. 455, n. 2, p. 419, doi. 10.1134/S1028334X14040096
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The stishovite paradox in the genesis of superdeep diamonds.
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- Doklady Earth Sciences, 2014, v. 455, n. 1, p. 274, doi. 10.1134/S1028334X14030064
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The phase diagram of Na carbonate, an alkaline component of the growth medium of ultradeep diamonds.
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- Doklady Earth Sciences, 2013, v. 453, n. 1, p. 1106, doi. 10.1134/S1028334X13110068
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The Na-Mg-Fe-Ti oxide mineral in association with picroilmenite and freudenbergite from kimberlite of the AK8 pipe, Botswana (natural and experimental data).
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- Doklady Earth Sciences, 2013, v. 451, n. 2, p. 849, doi. 10.1134/S1028334X13080084
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- Article
Congruent melting of calcium carbonate in a static experiment at 3500 K and 10-22 GPa: Its role in the genesis of ultradeep diamonds.
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- Doklady Earth Sciences, 2011, v. 439, n. 2, p. 1171, doi. 10.1134/S1028334X11080319
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New synthetic high-density nickel sulfide: A plausible component of the Earth’s core and terrestrial planets.
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- Doklady Earth Sciences, 2010, v. 432, n. 2, p. 771, doi. 10.1134/S1028334X10060139
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Synthesis and in-situ raman spectroscopy of nanodiamonds.
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- Doklady Physics, 2008, v. 53, n. 1, p. 1, doi. 10.1134/S1028335808010011
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Phase relations and formation of sodium-rich majoritic garnet in the system Mg<sub>3</sub>Al<sub>2</sub>Si<sub>3</sub>O<sub>12</sub>–Na<sub>2</sub>MgSi<sub>5</sub>O<sub>12</sub> at 7.0 and 8.5 GPa.
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- Contributions to Mineralogy & Petrology, 2008, v. 156, n. 2, p. 243, doi. 10.1007/s00410-008-0283-3
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Phase relations in the CaMgSi<sub>2</sub>O<sub>6</sub>-KAlSi<sub>3</sub>O<sub>8</sub> join at 6 and 3.5 GPa as a model for formation of some potassium-bearing deep-seated mineral assemblages.
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- Contributions to Mineralogy & Petrology, 2005, v. 149, n. 3, p. 316, doi. 10.1007/s00410-005-0651-1
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Modifiers of n-butyllithium in the synthesis of polybutadiene and styrene-butadiene rubbers.
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- International Polymer Science & Technology, 2014, v. 41, n. 3, p. 5, doi. 10.1177/0307174X1404100302
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- Article
Physicogeochemical Mechanisms of the Genesis of Matryoshka-Type Diamonds on the Basis of the Mantle-Carbonatite Theory.
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- Geochemistry International, 2023, v. 61, n. 3, p. 238, doi. 10.1134/S0016702923030072
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- Article
Peritectic Reaction of Olivine in the Olivine–Jadeite–Diopside–Garnet–(C–O–H) System at 6 GPa as the Key Mechanism of the Magmatic Evolution in the Upper Mantle.
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- Geochemistry International, 2021, v. 59, n. 9, p. 813, doi. 10.1134/S0016702921080048
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Physicogeochemical Evolution of Melts of Superplumes Uplift from the Lower Mantle to the Transition Zone: Experiment at 26 and 20 GPa.
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- Geochemistry International, 2021, v. 59, n. 7, p. 661, doi. 10.1134/S0016702921070041
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Genesis of Diamondiferous Rocks from Upper-Mantle Xenoliths in Kimberlite.
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- Geochemistry International, 2020, v. 58, n. 3, p. 245, doi. 10.1134/S0016702920030088
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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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The Role of Garnetization of Olivine in the Olivine–Diopside–Jadeite System in the Ultramafic–Mafic Evolution of Upper-Mantle Magmatism (Experiment at 6 GPa).
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- Geochemistry International, 2019, v. 57, n. 10, p. 1045, doi. 10.1134/S0016702919100070
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Genesis of Diamonds and Paragenetic Inclusions under Lower Mantle Conditions: The Liquidus Structure of the Parental System at 26 GPa.
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- Geochemistry International, 2019, v. 57, n. 2, p. 134, doi. 10.1134/S001670291902006X
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- Article
Interaction of Kimberlite Magma with Diamonds Upon Uplift from the Upper Mantle to the Earth’s Crust.
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- Geochemistry International, 2018, v. 56, n. 9, p. 881, doi. 10.1134/S0016702918090070
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Interaction of Titanium Minerals and Their Melts with Diamond-Forming Media (Experiments at 7-8 GPa).
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- Geochemistry International, 2018, v. 56, n. 2, p. 148, doi. 10.1134/S0016702918010032
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Magmatic evolution of the material of the Earth's lower mantle: Stishovite paradox and origin of superdeep diamonds (Experiments at 24-26 GPa).
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- Geochemistry International, 2016, v. 54, n. 11, p. 936, doi. 10.1134/S0016702916090032
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Fundamentals of the mantle carbonatite concept of diamond genesis.
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- Geochemistry International, 2016, v. 54, n. 10, p. 839, doi. 10.1134/S0016702916100086
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- Article
Phase relations in the system (Mg,Ca)AlSiO-NaMgSiO at 7.0 and 8.5 GPa and 1400-1900°C.
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- Geochemistry International, 2015, v. 53, n. 1, p. 9, doi. 10.1134/S0016702915010036
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Parental media of natural diamonds and primary mineral inclusions in them: Evidence from physicochemical experiment.
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- Geochemistry International, 2012, v. 50, n. 9, p. 726, doi. 10.1134/S0016702912070051
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Paragenetic relations of diamond with silicate and carbonate minerals in the carbonatite-diamond system: Experiments at 8.5 GPa.
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- Geochemistry International, 2012, v. 50, n. 3, p. 217, doi. 10.1134/S0016702912030093
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Mineral equilibria of diamond-forming carbonate-silicate systems.
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- Geochemistry International, 2011, v. 49, n. 13, p. 1267, doi. 10.1134/S0016702911130015
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