Characterization of Cu-mineralized carbonate veins in the Alta-Kvænangen Tectonic Window, Norway
The Alta-Kvænangen Tectonic Window is part of a regional greenstone belt that formed around 2.3 Ga – 2.0 Ga. The Bergmark anticline in the area has gone through greenschist to amphibolite facies metamorphism and hosts Cu, Co and Au mineralizations in hydrothermal veins, albite felsite and chemical t...
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Format: | Bachelor Thesis |
Language: | English |
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Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser
2024
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Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-104668 |