Geological setting and intrusion tectonics of the Kotalahti nickel-copper deposit, Finland
The wall rocks of the nickel bearing mafic and ultramafic plutonic rocks of Kotalahti are Archean banded granitoidic gneisses containing inliers of Archean metasediments and metavolcanics. The zircon ages of the granitoidic gneisses are around 2800 Ma. The zircons of the mafic plutonic rocks of the...
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| Format: | Article |
| Language: | English |
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Geological Society of Finland
1980-06-01
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| Series: | Bulletin of the Geological Society of Finland |
| Online Access: | http://www.geologinenseura.fi/bulletin/Volume52/sgs_bt_052_1_pages_101_128.pdf |