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...
Published in: | Minerals |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2018
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Subjects: | |
Online Access: | https://doi.org/10.3390/min8110474 |