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-...

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Bibliographic Details
Main Authors: Espen Torgerse, VIOLA, GIULIO
Other Authors: Viola, Giulio
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:http://hdl.handle.net/11585/569761