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


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2015-12

AUTHORS

N. G. Konopleva, G. Yu. Ivanyuk, Ya. A. Pakhomovsky, V. N. Yakovenchuk, Yu. A. Mikhailova, E. A. Selivanova

ABSTRACT

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. More... »

PAGES

614-625

Journal

TITLE

Geology of Ore Deposits

ISSUE

7

VOLUME

57

Author Affiliations

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s1075701515070065

DOI

http://dx.doi.org/10.1134/s1075701515070065

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1017533432


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