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...

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Bibliografski detalji
Glavni autori: E. Suikkanen, H. Huhma, M. Kurhila, Y. Lahaye
Format: Članak
Jezik:English
Izdano: Geological Society of Finland 2014-06-01
Serija:Bulletin of the Geological Society of Finland
Teme:
Online pristup:http://www.geologinenseura.fi/bulletin/Volume86/Bulletin_vol86_1_2014_Suikkanen.pdf