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- W2955243707 abstract "In order to model phlogopite formation in the upper-mantle garnet peridotites, it was performed an experimental study of the reaction En + 1/3Prp + [2/3KCl + 1/3H2O] = 1/3Phl + 1/3Cl-Phl in the presence of a H2O–KCl fluid with XKCl = 0.05–0.4 at pressure of 5 GPa and temperatures of 900–1250 °C. Experiments showed that the decrease of the Al content in orthopyroxene and the increase of the Cl content in phlogopite are good indicators of the KCl activity in the fluid. These relationships can be used to quantify the KCl activity during the metasomatic processes in the upper mantle." @default.
- W2955243707 created "2019-07-12" @default.
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- W2955243707 date "2019-04-24" @default.
- W2955243707 modified "2023-09-25" @default.
- W2955243707 title "Experimental Study of the Reaction Pyrope + Enstatite = Phlogopite in the Presence of H2O–KCl Fluid at 5 GPa in Application to the Problem of Modal Mantle Metasomatism" @default.
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- W2955243707 doi "https://doi.org/10.1007/978-3-030-00925-0_18" @default.
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