A. N. Kruk

发表

Carbonatite melt–peridotite interaction at 5.5–7.0 GPa: Implications for metasomatism in lithospheric mantle

A. Sokol, Y. Palyanov, A. N. Kruk, 2016 .

Melting experiments on the Udachnaya kimberlite at 6.3–7.5 GPa: Implications for the role of H2O in magma generation and formation of hydrous olivine

I. Kupriyanov, A. Sokol, N. Sobolev, 2013 .

Conditions of kimberlite magma generation: experimental constraints

A. Sokol, A. N. Kruk, 2015 .

Conditions of diamond crystallization in kimberlite melt: experimental data

A. Sokol, A. Khokhryakov, Y. Palyanov, 2015 .

The role of water in generation of group II kimberlite magmas: Constraints from multiple saturation experiments

A. Sokol, Y. Palyanov, A. N. Kruk, 2014 .

Stability of phlogopite in ultrapotassic kimberlite-like systems at 5.5–7.5 GPa

A. Sokol, N. Sobolev, Y. Palyanov, 2017, Contributions to Mineralogy and Petrology.

Phase relations in the Fe-Fe 3 C-Fe 3 N system at 7.8 GPa and 1350 °C: Implications for carbon and nitrogen hosts in Fe 0 -saturated upper mantle

A. Sokol, Y. Seryotkin, Y. Palyanov, 2017 .

The composition of garnet as an indicator of the conditions of peridotite-carbonatite interaction in the subcratonic lithosphere (experimental data)

A. Sokol, N. Sobolev, A. N. Kruk, 2015, Doklady Earth Sciences.

Cymrite as mineral clathrate: An overlooked redox insensitive transporter of nitrogen in the mantle

I. Kupriyanov, A. Sokol, Y. Seryotkin, 2020 .

Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts

A. Sokol, N. Sobolev, Y. Palyanov, 2015, Doklady Earth Sciences.

Conditions of phlogopite formation upon interaction of carbonate melts with peridotite of the subcratonic lithosphere

A. Sokol, N. Sobolev, A. N. Kruk, 2015, Doklady Earth Sciences.

The Fe–C–O–H–N system at 6.3–7.8 GPa and 1200–1400 °C: implications for deep carbon and nitrogen cycles

A. Sokol, Y. Seryotkin, A. Tomilenko, 2018, Contributions to Mineralogy and Petrology.

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

Yuri N. Palyanov, A. Sokol, N. Sobolev, 2017, Doklady Earth Sciences.

Fate of fluids at the base of subcratonic lithosphere: Experimental constraints at 5.5–7.8 GPa and 1150–1350 deg C

A. Sokol, A. Tomilenko, T. Bul’bak, 2018, Lithos.

Experimental Modeling of Diamond Resorption during Mantle Metasomatism

A. Sokol, D. V. Nechaev, A. Khokhryakov, 2022, Minerals.

Role of CO2 in the evolution of Kimberlite Magma: Experimental constraints at 5.5 GPa and 1200–1450 °C

A. Sokol, A. N. Kruk, 2021 .

Experimental Modeling of Decarbonation Reactions Resulting in Mg,Fe-garnets and CO2 fluid at the Mantle P–T parameters

O. Furman, I. Novoselov, A. N. Kruk, 2020 .

Phase relations in the Fe-Fe3C-Fe3N system at 7.8 GPa and 1150°C: implications for C and N hosts in metal-saturated mantle

A. Sokol, Y. Palyanov, A. N. Kruk, 2021, High Pressure Research.

Nitrogen storage capacity of phengitic muscovite and K-cymrite under the conditions of hot subduction and ultra high pressure metamorphism

I. Kupriyanov, A. Sokol, A. Korsakov, 2023, Geochimica et Cosmochimica Acta.

The effect of oxygen fugacity on diamond resorption in ascending kimberlite melt

A. Sokol, A. Khokhryakov, A. N. Kruk, 2021 .