Structural control and (re)mobilization of the extinct Haveri Au-Cu deposit, southern Finland
The extinct Haveri Au-Cu deposit is located within mafic metalavas and mafic/ intermediate banded rocks of the Haveri Formation, in the western part of the Paleoproterozoic Tampere Schist Belt. The sulfide-bearing banded rocks display a large E-W trending fold structure in magnetic and electromagnet...
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| Format: | Article |
| Language: | English |
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Geological Society of Finland
1994-06-01
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| Series: | Bulletin of the Geological Society of Finland |
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| Online Access: | http://www.geologinenseura.fi/bulletin/Volume66/sgs_bt_066_1_pages_039_044.pdf |