Abstract
The results of experimental studies are presented for reactions in the orthopyroxene–garnet–phlogopite system in the presence of H2O–KCl fluid at 3–5 GPa and 900–1000°C, which model the processes of phlogopite formation in garnet peridotites and pyroxenites during alkaline metasomatism of the upper mantle. The experiments demonstrated regular variations in the composition of garnet, pyroxenes, and phlogopite depending on the KCl content of the fluid. With increasing KCl content of the fluid, enstatite and garnet become unstable, the Al2O3 content of enstatite decreases, and the amount of grossular and knorringite components in garnet are maximum at a KCl content of ~10 mol %. Our results illustrate well the regular variations in the compositions of the coexisting minerals and their zoning in phlogopite-bearing peridotites of the lithospheric mantle.
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Funding
This work was supported by State Contracts nos. АААА–А18–118020590140–7 and АААА–А18–118020590148–3 of the Korzhinskii Institute of Experimental Mineralogy, Russian Academy of Sciences, for 2019–2021 and the Russian Foundation for Basic Research, project no. 18-05-00058.
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Translated by I. Melekestseva
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Limanov, E.V., Butvina, V.G., Safonov, O.G. et al. Phlogopite Formation in the Orthopyroxene–Garnet System in the Presence of H2O–KCl Fluid in Application to the Processes of Mantle Metasomatism. Dokl. Earth Sc. 494, 713–717 (2020). https://doi.org/10.1134/S1028334X20090111
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DOI: https://doi.org/10.1134/S1028334X20090111