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Gorbachev, N. S., Kostyuk, A. V., Shapovalov, Yu. B. (2015) Experimental study of the basalt–carbonate–H2O system at 4 GPa and 1100–1300°C: Origin of carbonatitic and high-K silicate magmas. Doklady Earth Sciences, 464 (2) 1018-1022 doi:10.1134/s1028334x15100037

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Reference TypeJournal (article/letter/editorial)
TitleExperimental study of the basalt–carbonate–H2O system at 4 GPa and 1100–1300°C: Origin of carbonatitic and high-K silicate magmas
JournalDoklady Earth Sciences
AuthorsGorbachev, N. S.Author
Kostyuk, A. V.Author
Shapovalov, Yu. B.Author
Year2015 (October)Volume464
Issue2
PublisherPleiades Publishing Ltd
DOIdoi:10.1134/s1028334x15100037Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID503520Long-form Identifiermindat:1:5:503520:9
GUID0
Full ReferenceGorbachev, N. S., Kostyuk, A. V., Shapovalov, Yu. B. (2015) Experimental study of the basalt–carbonate–H2O system at 4 GPa and 1100–1300°C: Origin of carbonatitic and high-K silicate magmas. Doklady Earth Sciences, 464 (2) 1018-1022 doi:10.1134/s1028334x15100037
Plain TextGorbachev, N. S., Kostyuk, A. V., Shapovalov, Yu. B. (2015) Experimental study of the basalt–carbonate–H2O system at 4 GPa and 1100–1300°C: Origin of carbonatitic and high-K silicate magmas. Doklady Earth Sciences, 464 (2) 1018-1022 doi:10.1134/s1028334x15100037
In(2015, October) Doklady Earth Sciences Vol. 464 (2) Pleiades Publishing Ltd

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Gorbachev, N. S., Shapovalov, Yu. B., Kostyuk, A. V. (2017) Experimental study of the apatite–carbonate–H2O system at P = 0.5 GPa and T = 1200°C: Efficiency of fluid transport in carbonatite. Doklady Earth Sciences, 473 (1) 350-353 doi:10.1134/s1028334x17030230
Gorbachev, N. S., Kostyuk, A. V., Shapovalov, Yu. B. (2015) Experimental study of the peridotite-H2O system at P = 3.8–4 GPa and T = 1000–1400°C: Critical relations and vertical zoning of the upper mantle. Doklady Earth Sciences, 461 (2) 360-363 doi:10.1134/s1028334x15040017
Gorbachev, N. S., Shapovalov, Yu. B., Kostyuk, A. V. (2018) The Influence of Sodium and Potassium Chlorides on Phase Ratios in the Eclogite–CaCO3–H2O + CO2 System at 4 GPa and 1200–1300°C. Doklady Earth Sciences, 479 (2) 524-528 doi:10.1134/s1028334x18040232
Gorbachev, N. S., Shapovalov, Yu. B., Kostyuk, A. V. (2017) Experimental study of eclogitization and melting of basic rocks at Р = 4 GPa and Т = 1200–1400°С. Doklady Earth Sciences, 474 (2) 695-699 doi:10.1134/s1028334x17060198
Gorbachev, N. S., Shapovalov, Yu. B., Kostyuk, A. V., Gorbachev, P. N., Nekrasov, A. N. (2024) Phase Relationships and Distribution of S, Fe, Co, Ni, Re, Os, and Pt between Metal and Sulfide Melts in the Basalt–Fe–FeS–C System at 1400°C and 4 GPa. Doklady Earth Sciences, 519 (2). doi:10.1134/s1028334x24603092
Gorbachev, N. S., Kostyuk, A. V., Shapovalov, Yu. B., Gorbachev, P. N., Nekrasov, A. N., Soultanov, D. M. (2019) Critical Phenomena and Garnetization of Hydrous Eclogite at P = 3.7–4.0 GPa and T = 1000–1300°C. Doklady Earth Sciences, 489 (2) 1421-1425 doi:10.1134/s1028334x19120031
Gorbachev, N. S., Kostyuk, A. V., Shapovalov, Yu. B., Gorbachev, P. N., Nekrasov, A. N., Soultanov, D. M. (2019) Phase Relations upon the Interaction of Phlogopite with a Carbonate Melt at P = 3.8 GPa. Doklady Earth Sciences, 488 (2) 1240-1244 doi:10.1134/s1028334x19100210
Gorbachev, N. S., Shapovalov, Yu. B., Kostyuk, A. V., Gorbachev, P. N., Nekrasov, A. N., Soultanov, D. M. (2021) Phase Relations in the Fe–S–C System at P = 0.5 GPa, T = 1100–1250°C: Fe–S–C Liquation and Its Role in the Formation of Magmatic Sulfide Deposits. Doklady Earth Sciences, 497 (1) 206-210 doi:10.1134/s1028334x21030028
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Gorbachev, N. S., Kostyuk, A. V., Nekrasov, A. N., Gorbachev, P. N., Sultanov, D. M. (2019) Experimental Study of the Peridotite–Basalt–Fluid System: Phase Relations at Subcritical and Supercritical Р-Т Conditions. Petrology, 27 (6) 553-566 doi:10.1134/s0869591119060031
Bobrov, A. V., Dymshits, A. M., Litvin, Yu. A. (2009) The pyrope Mg3Al2Si3O12-jadeite NaAlSi2O6 system: An experimental study at 7.0 and 8.5 GPa and 1300–1900°C. Doklady Earth Sciences, 426 (1) 672-676 doi:10.1134/s1028334x09040369
 
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