Vanadium Mineralization in the Kola Region, Fennoscandian Shield

In the northern Fennoscandian Shield, vanadium mineralization occurs in the Paleoproterozoic Pechenga–Imandra-Varzuga (PIV) riftogenic structure. It is localized in sulfide ores hosted by sheared basic and ultrabasic metavolcanics in the Pyrrhotite Ravine and Bragino areas and was formed at the late...

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Bibliographic Details
Published in:Minerals
Main Authors: Alena A. Kompanchenko, Anatoly V. Voloshin, Victor V. Balagansky
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
Online Access:https://doi.org/10.3390/min8110474