Role of Liquid Immiscibility in the Formation of the Rare Metal Granites of the Katugin Massif, Aldan Shield
The paper discusses possible immiscibility between fluoride salt (“cryolite”) and silicate liquids into which the parental melt of the Katugin massif exsolves, and the petrological implications of this phenomenon. Results of a detailed study of the cryolite and zircon are presented. Liquid immiscibi...
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| Veröffentlicht in: | Petrology 2024-08, Vol.32 (4), p.551-568 |
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| creator | Tolmacheva, E. V. Velikoslavinskii, S. D. Kotov, A. B. Larin, A. M. Sklyarov, E. V. Gladkochub, D. P. Donskaya, T. V. Skovitina, T. M. Kovach, V. P. Galankina, O. L. |
| description | The paper discusses possible immiscibility between fluoride salt (“cryolite”) and silicate liquids into which the parental melt of the Katugin massif exsolves, and the petrological implications of this phenomenon. Results of a detailed study of the cryolite and zircon are presented. Liquid immiscibility is demonstrated to have triggered the massive crystallization of zircon and, together with the processes of subsequent evolution of the cryolite melt, contributed to the formation of the large cryolite bodies. Data on mineral-hosted inclusions were used to estimate the crystallization temperatures of fluoride salt and silicate melts and outline the pathways of their evolution during the formation of the massif. It is shown that the granites of the Katugin and West Katugin massifs were most likely derived from distinct sources, that differed mainly in fluorine content. Data on the chemical composition of three zircon generations identified in the granites of the Katugin massif are presented. |
| doi_str_mv | 10.1134/S0869591124700127 |
| format | Article |
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V. ; Velikoslavinskii, S. D. ; Kotov, A. B. ; Larin, A. M. ; Sklyarov, E. V. ; Gladkochub, D. P. ; Donskaya, T. V. ; Skovitina, T. M. ; Kovach, V. P. ; Galankina, O. L.</creator><creatorcontrib>Tolmacheva, E. V. ; Velikoslavinskii, S. D. ; Kotov, A. B. ; Larin, A. M. ; Sklyarov, E. V. ; Gladkochub, D. P. ; Donskaya, T. V. ; Skovitina, T. M. ; Kovach, V. P. ; Galankina, O. L.</creatorcontrib><description>The paper discusses possible immiscibility between fluoride salt (“cryolite”) and silicate liquids into which the parental melt of the Katugin massif exsolves, and the petrological implications of this phenomenon. Results of a detailed study of the cryolite and zircon are presented. Liquid immiscibility is demonstrated to have triggered the massive crystallization of zircon and, together with the processes of subsequent evolution of the cryolite melt, contributed to the formation of the large cryolite bodies. Data on mineral-hosted inclusions were used to estimate the crystallization temperatures of fluoride salt and silicate melts and outline the pathways of their evolution during the formation of the massif. It is shown that the granites of the Katugin and West Katugin massifs were most likely derived from distinct sources, that differed mainly in fluorine content. Data on the chemical composition of three zircon generations identified in the granites of the Katugin massif are presented.</description><identifier>ISSN: 0869-5911</identifier><identifier>EISSN: 1556-2085</identifier><identifier>DOI: 10.1134/S0869591124700127</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Chemical composition ; Cryolite ; Crystallization ; Earth and Environmental Science ; Earth Sciences ; Evolution ; Fluorides ; Fluorine ; Fluorine content ; Geochemistry ; Granite ; Immiscibility ; Inclusions ; Liquids ; Massifs ; Melts (crystal growth) ; Mineralogy ; Miscibility ; Silicates ; Zircon</subject><ispartof>Petrology, 2024-08, Vol.32 (4), p.551-568</ispartof><rights>Pleiades Publishing, Ltd. 2024. 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Data on mineral-hosted inclusions were used to estimate the crystallization temperatures of fluoride salt and silicate melts and outline the pathways of their evolution during the formation of the massif. It is shown that the granites of the Katugin and West Katugin massifs were most likely derived from distinct sources, that differed mainly in fluorine content. 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| source | Springer Nature - Complete Springer Journals |
| subjects | Chemical composition Cryolite Crystallization Earth and Environmental Science Earth Sciences Evolution Fluorides Fluorine Fluorine content Geochemistry Granite Immiscibility Inclusions Liquids Massifs Melts (crystal growth) Mineralogy Miscibility Silicates Zircon |
| title | Role of Liquid Immiscibility in the Formation of the Rare Metal Granites of the Katugin Massif, Aldan Shield |
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