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Sokol, Alexander G., Kruk, Alexey N., Chebotarev, Dimity A., Palyanov, Yury N. (2016) Carbonatite melt–peridotite interaction at 5.5–7.0 GPa: Implications for metasomatism in lithospheric mantle. Lithos, 248. 66-79 doi:10.1016/j.lithos.2016.01.013

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Reference TypeJournal (article/letter/editorial)
TitleCarbonatite melt–peridotite interaction at 5.5–7.0 GPa: Implications for metasomatism in lithospheric mantle
JournalLithos
AuthorsSokol, Alexander G.Author
Kruk, Alexey N.Author
Chebotarev, Dimity A.Author
Palyanov, Yury N.Author
Year2016 (April)Volume248
PublisherElsevier BV
DOIdoi:10.1016/j.lithos.2016.01.013Search in ResearchGate
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Mindat Ref. ID275859Long-form Identifiermindat:1:5:275859:0
GUID0
Full ReferenceSokol, Alexander G., Kruk, Alexey N., Chebotarev, Dimity A., Palyanov, Yury N. (2016) Carbonatite melt–peridotite interaction at 5.5–7.0 GPa: Implications for metasomatism in lithospheric mantle. Lithos, 248. 66-79 doi:10.1016/j.lithos.2016.01.013
Plain TextSokol, Alexander G., Kruk, Alexey N., Chebotarev, Dimity A., Palyanov, Yury N. (2016) Carbonatite melt–peridotite interaction at 5.5–7.0 GPa: Implications for metasomatism in lithospheric mantle. Lithos, 248. 66-79 doi:10.1016/j.lithos.2016.01.013
In(2016) Lithos Vol. 248. Elsevier BV

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Sokol, Alexander G., Kruk, Alexey N. (2021) Role of CO2 in the evolution of Kimberlite Magma: Experimental constraints at 5.5 GPa and 1200–1450 °C. Lithos, 386. 106042pp. doi:10.1016/j.lithos.2021.106042
Sokol, Alexander G., Kruk, Alexey N., Palyanov, Yury N., Sobolev, Nikolay V. (2017) Stability of phlogopite in ultrapotassic kimberlite-like systems at 5.5–7.5 GPa. Contributions to Mineralogy and Petrology, 172 (4) doi:10.1007/s00410-017-1341-5
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Sokol, A. G., Kruk, A. N., Chebotarev, D. A., Palyanov, Yu. N., Sobolev, N. V. (2015) Conditions of carbonation and wehrlitization of lithospheric peridotite upon interaction with carbonatitic melts. Doklady Earth Sciences, 465 (2) 1262-1267 doi:10.1134/s1028334x15120144
Kruk, A. N., Sokol, A. G., Palyanov, Yu. N. (2018) Phase Relations in the Harzburgite–Hydrous Carbonate Melt at 5.5–7.5 GPa and 1200–1350°С. Petrology, 26 (6) 575-587 doi:10.1134/s0869591118060036
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