Kalsilite of the Khibiny and Lovozero alkaline plutons, Kola Peninsula

被引：0

作者：

Ya. A. Pakhomovsky

V. N. Yakovenchuk

G. Yu. Ivanyuk

机构：

[1] Russian Academy of Sciences,Geological Institute, Kola Science Center

来源：

Geology of Ore Deposits | 2009年 / 51卷

关键词：

Nepheline; Kola Peninsula; Nepheline Syenite; Aegirine; Alkaline Pluton;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

Kalsilite—a typical mineral of ore-bearing zones of the Khibiny and Lovozero plutons—was formed after low-Si and high-K nepheline in one of three ways: (1) by relatively high-temperature replacement of Na with K; (2) due to orthoclase-kalsilite poikiloblastesis in foidolites and overlapping foyaites; or (3) by replacement of nepheline with zeolite.

引用

页码：822 / 826

页数：4

共 16 条

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[9]

Konopleva N. G.(undefined)undefined undefined undefined undefined-undefined

[10]

Ivanyuk G. Yu.(undefined)undefined undefined undefined undefined-undefined

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