The sulphides that were mined was found in Mo-Cu bearing quartz veins in quartzites and metabasic volcanics of the Bandak group in the precambrian rocks of the Telemark suite.
Ref.:
- Hasan, Zia-Ul (1971): Precambrian rocks of the Telemark area in south central Norway XI: Supracrustal rocks and Mo-Cu bearing veins in Dalen. Norsk Geologisk Tidsskrift 51, 287-309
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