Formation mechanism of the Vaasa Batholith in the Fennoscandian shield: Petrographic and geochemical constraints
The ~1.88 Ga Vaasa Batholith in western Finland is a large granitoid area (8 000 km2) with gradational contacts against the garnet- and cordierite-bearing diatexite and metatexite migmatites of the Pohjanmaa Belt. It is located in the middle part of the Fennoscandian Shield and was formed during the...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Geological Society of Finland
2012-12-01
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| Series: | Bulletin of the Geological Society of Finland |
| Subjects: | |
| Online Access: | http://www.geologinenseura.fi/bulletin/Volume84/Makitie2012.pdf |