Ulvöspinel from xenoliths of contact-altered volcanic and volcanosedimentary rocks in nepheline syenites of the Khibiny and Lovozero plutons View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2012-12

AUTHORS

G. Yu. Ivanyuk, Yu. A. Korchak, Ya. A. Pakhomovsky, Yu. P. Men’shikov, V. N. Yakovenchuk

ABSTRACT

Ulvöspinel is a typical accessory mineral of xenoliths of volcanic and volcanosedimentary rocks in alkaline syenites of the Khibiny and Lovozero plutons. Ulvöspinel forms homogeneous Cr- and V-rich grains in slightly altered olivine basalts, basaltic tuffs, and tuffites and is enriched in Mn and Si in the course of contact-metasomatic alteration of these rocks. The strongly reduced conditions of contact metamorphism controlled by ascending flows of hydrocarbon gases and hydrogen sulfide gave rise to the subsolidus decomposition of primary ulvöspinel and Ti-high magnetite with the formation of ilmenite lamellae and then, with decreasing redox potential, of the second-generation latticed ulvöspinel lamellae. More... »

PAGES

575-579

References to SciGraph publications

Journal

TITLE

Geology of Ore Deposits

ISSUE

7

VOLUME

54

Author Affiliations

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s107570151108006x

DOI

http://dx.doi.org/10.1134/s107570151108006x

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1024204166


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