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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Bibliographic Details
Main Author: Svens, Ellen
Format: Bachelor Thesis
Language:English
Published: Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser 2024
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-104668