Structural and magmatic evolution in the Loimaa area, southwestern Finland
Within the Loimaa area there is a junction of the general E-W structural trend of southern Finland and a NW-N-NE curving trend. The structure of the area is dominated by ductile D3 and D4 deformations with E-W and N-S axial traces, respectively. The typical semicircular structures in the study area...
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| Format: | Article |
| Language: | English |
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Geological Society of Finland
1999-06-01
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| Series: | Bulletin of the Geological Society of Finland |
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| Online Access: | http://www.geologinenseura.fi/bulletin/Volume71/sgs_bt_071_1_pages_057_071.pdf |