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作者:M. Kurhila , P. Hölttä
来源:[J].Bulletin of the Geological Society of Finland(IF 0.786), 2016, Vol.88 (1), pp.5-20DOAJ
摘要:The Vaasa batholith, western Finland, is a large, peraluminous granitoid pluton that crystallized at 1.88–1.87 Ga during the culmination of the Svecofennian orogeny. The batholith has gradual contacts, through metatexites and diatexites, with the enveloping metasedimentary r...

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