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Degassing Mechanisms of Kimberlite Magma at Its Initial Ascent: Experimental Data at 5.5 and 3.0 GPa

Geochemistry international, 2022-11, Vol.60 (11), p.1087-1102

2022

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Erratum to: Stability of Carbonates during Subduction: Influence of the Dehydration Regime of Chlorine-Bearing Metapelite

Doklady earth sciences, 2023-11, Vol.513 (1), p.1261-1261

2023

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Stability of Carbonates during Subduction: Influence of the Dehydration Regime of Chlorine-Bearing Metapelite

Doklady earth sciences, 2023-05, Vol.509 (1), p.139-143

2023

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Dissolution of Peridotite in a Volatile-Rich Carbonate Melt as a Mechanism of the Formation of Kimberlite-like Melts (Experimental Constraints)

Doklady earth sciences, 2022-04, Vol.503 (2), p.157-163

2022

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Composition of primary kimberlite magma: constraints from melting and diamond dissolution experiments

Contributions to mineralogy and petrology, 2015-09, Vol.170 (3), p.85-18, Article 26

2015

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Viscosity of Depolymerized Dunite Melts under Medium and High Pressures

Geochemistry international, 2018-12, Vol.56 (12), p.1148-1155

2018

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Synthesis of NH4-Substituted Muscovite at 6.3 GPa and 1000°C: Implications for Nitrogen Transport to the Earth’s Mantle

Doklady earth sciences, 2018-03, Vol.479 (1), p.404-407

2018

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Diamond Crystallization from a Sulfur−Carbon System at HPHT Conditions

Crystal growth & design, 2009-06, Vol.9 (6), p.2922-2926

2009

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Diamond formation from mantle carbonate fluids

Nature (London), 1999-07, Vol.400 (6743), p.417-418

1999

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Trace-element mobility in pelite-derived supercritical fluid-melt at subduction-zone conditions

Contributions to mineralogy and petrology, 2024-05, Vol.179 (5), p.50, Article 50

2024

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Composition of the fluid in carbonate- and chlorine-bearing pelite near the second critical point; results of diamond trap experiments

Russian geology and geophysics, 2023-08, Vol.64 (8), p.919-931

2023

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Viscosity of hydrous kimberlite and basaltic melts at high pressures

Russian geology and geophysics, 2017-09, Vol.58 (9), p.1093-1100

2017

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Composition of reduced mantle fluids; evidence from modeling experiments and fluid inclusions in natural diamond

Russian geology and geophysics, 2020-05, Vol.61 (5-6), p.663-674

2020

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Conditions of diamond crystallization in kimberlite melt: experimental data

Russian geology and geophysics, 2015-01, Vol.56 (1-2), p.196-210

2015

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Conditions for the origin of oxidized carbonate-silicate melts: Implications for mantle metasomatism and diamond formation

Lithos, 2012, Vol.128, p.113-125

2012

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Diamond formation in the system MgO–SiO2–H2O–C at 7.5 GPa and 1,600°C

Contributions to mineralogy and petrology, 2008, Vol.155 (1), p.33-43

2008

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Conditions of formation of Cr-pyrope and escolaite during mantle metasomatism: Experimental modeling

Doklady earth sciences, 2012, Vol.442 (1), p.76-80

2012

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Phase Relations in the Harzburgite–Hydrous Carbonate Melt at 5.5–7.5 GPa and 1200–1350°С

Petrology, 2018-11, Vol.26 (6), p.575-587

2018

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Synthesis of hydrocarbons by CO2 fluid conversion with hydrogen: Experimental modeling at 7.8 GPa and 1350°C

Doklady earth sciences, 2017-12, Vol.477 (2), p.1483-1487

2017

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Conditions of kimberlite magma generation: experimental constraints

Russian geology and geophysics, 2015-01, Vol.56 (1-2), p.245-259

2015

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Formation of Water-Bearing Defects in Olivine in the Presence of Water–Hydrocarbon Fluid at 6.3 GPa and 1200°C

Doklady earth sciences, 2018-12, Vol.483 (1), p.1451-1453

2018

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Change in the viscosity of kimberlite and basaltic magmas during their origin and evolution (prediction)

Russian geology and geophysics, 2015-06, Vol.56 (6), p.885-892

2015

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Phases of the Fe–C–N system as hosts of mantle carbon and nitrogen: Experimental studies at 7.8 GPa and 1350°C

Doklady earth sciences, 2017-07, Vol.475 (1), p.780-783

2017

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The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: experimental modeling under PT-conditions of lithospheric mantle

Russian geology and geophysics, 2015-01, Vol.56 (1-2), p.143-154

2015

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Stability of methane in reduced C–O–H fluid at 6.3 GPa and 1300–1400°C

Doklady earth sciences, 2017-06, Vol.474 (2), p.680-683

2017

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Degassing Mechanisms of Kimberlite Magma at Its Initial Ascent: Experimental Data at 5.5 and 3.0 GPa

Erratum to: Stability of Carbonates during Subduction: Influence of the Dehydration Regime of Chlorine-Bearing Metapelite

Stability of Carbonates during Subduction: Influence of the Dehydration Regime of Chlorine-Bearing Metapelite

Dissolution of Peridotite in a Volatile-Rich Carbonate Melt as a Mechanism of the Formation of Kimberlite-like Melts (Experimental Constraints)

Composition of primary kimberlite magma: constraints from melting and diamond dissolution experiments

Viscosity of Depolymerized Dunite Melts under Medium and High Pressures

Synthesis of NH4-Substituted Muscovite at 6.3 GPa and 1000°C: Implications for Nitrogen Transport to the Earth’s Mantle

Diamond Crystallization from a Sulfur−Carbon System at HPHT Conditions

Diamond formation from mantle carbonate fluids

Trace-element mobility in pelite-derived supercritical fluid-melt at subduction-zone conditions

Composition of the fluid in carbonate- and chlorine-bearing pelite near the second critical point; results of diamond trap experiments

Viscosity of hydrous kimberlite and basaltic melts at high pressures

Composition of reduced mantle fluids; evidence from modeling experiments and fluid inclusions in natural diamond

Conditions of diamond crystallization in kimberlite melt: experimental data

Conditions for the origin of oxidized carbonate-silicate melts: Implications for mantle metasomatism and diamond formation

Diamond formation in the system MgO–SiO2–H2O–C at 7.5 GPa and 1,600°C

Conditions of formation of Cr-pyrope and escolaite during mantle metasomatism: Experimental modeling

Phase Relations in the Harzburgite–Hydrous Carbonate Melt at 5.5–7.5 GPa and 1200–1350°С

Synthesis of hydrocarbons by CO2 fluid conversion with hydrogen: Experimental modeling at 7.8 GPa and 1350°C

Conditions of kimberlite magma generation: experimental constraints

Formation of Water-Bearing Defects in Olivine in the Presence of Water–Hydrocarbon Fluid at 6.3 GPa and 1200°C

Change in the viscosity of kimberlite and basaltic magmas during their origin and evolution (prediction)

Phases of the Fe–C–N system as hosts of mantle carbon and nitrogen: Experimental studies at 7.8 GPa and 1350°C

The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: experimental modeling under PT-conditions of lithospheric mantle

Stability of methane in reduced C–O–H fluid at 6.3 GPa and 1300–1400°C

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