Abstract
At 750°C and a pressure of 1 kbar, an experiment was carried out simulating the contact-reaction interaction of calcite and a highly evolved fluorine-containing granite melt. The water content in the system did not exceed 10% of the dry charge mass. The possibility of interaction between magmatic melt and calcite is shown. The experimental products contain a zoned column composed of liquid phases and crystalline minerals. In the apocarbonate part, the newly formed phases are cuspidine, quartz, wollastonite, grossular, and a non-crystalline carbonate–fluoride phase LCF. The mineral assemblages in the zones of the apocarbonate part of the column vary depending on the ratio of CO2 and HF activities. In the silicate part, aluminosilicate glass, alkali feldspar, and plagioclase of variable composition were found. Silicon and fluorine are intensively transferred from the silicate to carbonate part, and a small amount of calcium is transferred in the opposite direction.
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ACKNOWLEDGEMENTS
The authors thank V.A. Popov, T.I. Shchekina, A.R. Kotel’nikov, and B.B. Shkurskii for discussing the results and valuable comments on the manuscript.
Funding
This work was supported by ongoing institutional funding under the research project “Petrogenetic Regimes in the Inner Geospheres of the Earth”. No additional grants to carry out or direct this particular research were obtained. The analytical data were obtained at the Laboratory of Analytical Techniques of High Spatial Resolution at the Department of Petrology and Volcanology, Geological Faculty, Moscow State University, with the use of a JEOL JXA-8230 microprobe that had been purchased under the Development Program for the Moscow State University.
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Alferyeva, Y.O., Gramenitsky, E.N. & Novikova, A.S. Experimental Modeling of Interaction between Fluorine-Containing Granite Melt and Calcite Marble. Petrology 32, 236–248 (2024). https://doi.org/10.1134/S0869591124020024
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DOI: https://doi.org/10.1134/S0869591124020024