Phanerozoic veins of galena in the Åland rapakivi area, southwestern Finland
Some minor galena mineralizations are in part associated with clastic dykes of Cambrian sandstone in the Aland rapakivi area. Galena also occurs disseminated in greisen-type mineralizations. The difference in age between the two modes of occurrence is probably at least 1100 Ma. No traces of a magmat...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Geological Society of Finland
1979-12-01
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| Series: | Bulletin of the Geological Society of Finland |
| Online Access: | http://www.geologinenseura.fi/bulletin/Volume51/sgs_bt_051_pages_055_062.pdf |