Kalsilite of the Khibiny and Lovozero alkaline plutons, Kola Peninsula View Full Text


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Article Info

DATE

2009-12

AUTHORS

Ya. A. Pakhomovsky, V. N. Yakovenchuk, G. Yu. Ivanyuk

ABSTRACT

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.

PAGES

822-826

References to SciGraph publications

Journal

TITLE

Geology of Ore Deposits

ISSUE

8

VOLUME

51

Author Affiliations

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s1075701509080157

DOI

http://dx.doi.org/10.1134/s1075701509080157

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1018677876


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