Evolution of metal-bearing fluids at the Nussir and Ulveryggen sediment-hosted Cu deposits, Repparfjord Tectonic Window, northern Norway

The Palaeoproterozoic greenstone belts of Fennoscandia are metamorphosed and deformed volcanic and sedimentary rocks that formed in basins with a high base-metal ore potential. One of these, the Repparfjord Tectonic Window (RTW), is exposed in the Caledonides of northern Norway and contains several...

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Bibliographic Details
Published in:Norwegian Journal of Geology
Main Authors: Mun, Yulia, Strmic Palinkas, Sabina, Kullerud, Kåre, Nilsen, Kjell S., Neufeld, Kai, Bekker, Andrey
Format: Article in Journal/Newspaper
Language:English
Published: Norsk Geologisk Forening 2020
Subjects:
Online Access:https://hdl.handle.net/10037/20062
https://doi.org/10.17850/njg100-2-5