Composition and conditions of crystallization of zircon from the rare-metal ores of the Gremyakha–Vyrmes Massif, Kola Peninsula
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- 作者：N. V. Sorokhtina ; L. N. Kogarko ; A. K. Shpachenko…
- 关键词：zircon ; rare ; metal ores ; alkaline rocks ; Gremyakha–Vyrmes Massif ; Kola Peninsula
- 刊名：Geochemistry International
- 出版年：2016
- 出版时间：December 2016
- 年：2016
- 卷：54
- 期：12
- 页码：1035-1048
- 全文大小：
- 刊物主题：Geochemistry;
- 出版者：Pleiades Publishing
- ISSN：1556-1968
- 卷排序：54
文摘
The first data on the composition and inner structure of zircon, one of the main ore minerals of the rare-metal metasomatites of the Gremyakha–Vyrmes alkaline-ultramafic massif, are reported. Early zircon generations are enriched in Y and REE and contain numerous inclusions of rock-forming and accessory minerals of metasomatites, as well as syngenetic fluid inclusions of calcite, thorite and thorianite. Late generations differ in the elevated Hf content and contain no inclusions. The elevated concentrations of Ca and Th in the central zones of crystals are related to the presence of numerous micron-sized inclusions of calcite and thorium phases. All zircon varieties have extremely low U and Pb contents. Concentrations and distribution patterns of incompatible and rare-earth elements in zircon from the metasomatites of the Gremyakha–Vyrmes Massif are similar to those of syenite pegmatites and magmatic carbonatites around the world. Mineral from these associations shows a positive Ce anomaly and elevated HREE contents. According to the compositions of zircon and thorite inclusion in it and experimental data on the simultaneous synthesis of these minerals, the crystallization temperature of zircon was 700–750°С. Using Ti-in-zircon temperature dependence, late zurcon was formed at temperature of 700–750°С. The rare-metal metasomatites are formed at the final stages of the massif formation, presumably after foidolites. Carbonatites could initiate metasomatic reworking of foidolites and accumulation of trace metals in them. The evolution of the primary alkaline–ultramafic melt toward the enrichment in trace elements was mainly controlled by crystallization differentiation.