Revised structure and stratigraphy of the northwestern Repparfjord Tectonic Window, northern Norway
The Repparfjord Tectonic Window (RTW) consists of a ~8 km-thick low-grade, weakly deformed Early Palaeoproterozoic volcano-sedimentary succession that hosts abundant Cu mineralisations. Two major, sediment-hosted, Cu-deposits occur in the Saltvatnet Group, a <6 km-thick sequence of mainly coarse-...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2015
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Online Access: | http://hdl.handle.net/11585/569761 |