Typochemistry of rinkite and products of its alteration in the Khibiny Alkaline pluton, Kola Peninsula

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• 作者：N. G. Konopleva ; G. Yu. Ivanyuk ; Ya. A. Pakhomovsky…
• 刊名：Geology of Ore Deposits
• 出版年：2015
• 出版时间：December 2015
• 年：2015
• 卷：57
• 期：7
• 页码：614-625
• 全文大小：1,969 KB
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• 作者单位：N. G. Konopleva (1)
  G. Yu. Ivanyuk (1) (2)
  Ya. A. Pakhomovsky (1) (2)
  V. N. Yakovenchuk (1) (2)
  Yu. A. Mikhailova (1) (2)
  E. A. Selivanova (1) (2)
  
  1. Nanomaterials Research Center, Kola Science Center, Russian Academy of Sciences, Apatity, Murmansk oblast, 184209, Russia
  2. Geological Institute. Kola Science Center, ul. Fersmana 14, Apatity, Murmansk oblast, 184209, Russia
  
• 刊物主题：Mineral Resources;
• 出版者：Springer US
• ISSN：1555-6476

文摘

The occurrence, morphology, and composition of rinkite are considered against the background of zoning in the Khibiny pluton. Accessory rinkite is mostly characteristic of foyaite in the outer part of pluton, occurs somewhat less frequently in foyaite and rischorrite in the central part of pluton, even more sparsely in foidolites and apatite–nepheline rocks, and sporadically in fenitized xenoliths of the Lovozero Formation. The largest, up to economic, accumulations of rinkite are related to the pegmatite and hydrothermal veins, which occur in nepheline syenite on both sides of the Main foidolite ring. The composition of rinkite varies throughout the pluton. The Ca, Na, and F contents in accessory rinkite and amorphous products of its alteration progressively increase from foyaite and fenitized basalt of the Lovozero Formation to foidolite, rischorrite, apatite–nepheline rocks, and pegmatite–hydrothermal veins.