Hydrothermal alteration of the Kemi layered intrusion
Abstract. The Kemi chromite deposit is located near the towns of Kemi and Tornio (northern Finland). The mineralization is hosted within the mafic-ultramafic Kemi intrusion (~2.4 Ga) that is part of the Tornio–Näränkävaara belt. The main chromite zone is located in the basal part of the intrusion an...
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| Format: | Master Thesis |
| Language: | English |
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University of Oulu
2019
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| Online Access: | http://jultika.oulu.fi/Record/nbnfioulu-201904241520 |