The age and origin of the Vaasa migmatite complex revisited
The origin of the Vaasa migmatite complex was studied by using whole-rock Sm-Nd and zircon Lu-Hf and U-Pb data in conjunction with whole-rock major and trace element geochemistry. The concordia ages of five Vaasa area granitoid samples are 1.88–1.86 Ga, constraining the age of peak migmatization. Th...
Glavni autori: | , , , |
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Format: | Članak |
Jezik: | English |
Izdano: |
Geological Society of Finland
2014-06-01
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Serija: | Bulletin of the Geological Society of Finland |
Teme: | |
Online pristup: | http://www.geologinenseura.fi/bulletin/Volume86/Bulletin_vol86_1_2014_Suikkanen.pdf |