Late Palaeozoic fault-controlled hydrothermal Cu–Zn mineralisation on Vanna island, West Troms Basement Complex, northern Norway

The Vannareid–Burøysund fault is a major, brittle, normal fault in northern Norway, with cohesive fault rocks (cataclasites) that host Cu–Zn-bearing quartz-carbonate veins. The fault is exposed on the island of Vanna in the Neoarchaean to Palaeoproterozoic West Troms Basement Complex, separating var...

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Bibliographic Details
Published in:Norwegian Journal of Geology
Main Authors: Paulsen, Hanne-Kristin, Bergh, Steffen G, Strmic Palinkas, Sabina
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of Norway 2020
Subjects:
Online Access:https://hdl.handle.net/10037/18644
https://doi.org/10.17850/njg100-1-2