Minerals of zirconolite group from fenitized xenoliths in nepheline syenites of Khibiny and Lovozero plutons, Kola Peninsula View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2015-12

AUTHORS

Yu. P. Menshikov, Yu. A. Mikhailova, Ya. A. Pakhomovsky, V. N. Yakovenchuk, G. Yu. Ivanyuk

ABSTRACT

Zirconolite, its Ce-, Nd-, and Y-analogs, and laachite, another member of the zirconolite group, are typomorphic minerals of the fenitized xenoliths in nepheline syenite and foidolite of the Khibiny–Lovozero Complex, Kola Peninsula, Russia. All these minerals are formed at the late stage of fenitization as products of ilmentie alteration under the effect of Zr-bearing fluids. The diversity of these minerals is caused by the chemical substitutions of Na and Ca for REE, Th, and U compensated by substitution of Ti and Zr for Nb, Fe and Ta, as well as by the redistribution of REE between varieties enriched in Ti (HREE) or Nb (LREE). The results obtained can be used in the synthesis of Synroc-type titanate ceramics assigned for the immobilization of actinides. More... »

PAGES

591-599

Journal

TITLE

Geology of Ore Deposits

ISSUE

7

VOLUME

57

Author Affiliations

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s1075701515070089

DOI

http://dx.doi.org/10.1134/s1075701515070089

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1026681688


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