The Orivesi granite batholith, Southern Central Finland - characteristics and emplacement
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چکیده
منابع مشابه
Granite: From genesis to emplacement
At low temperatures (<750 °C at moderate to high crustal pressures), the production of suffi cient melt to reach the melt connectivity transition (~7 vol%), enabling melt drainage, requires an infl ux of aqueous fl uid along structurally controlled pathways or recycling of fl uid via migration of melt and exsolution during crystallization. At higher temperatures, melting occurs by fl uid-absent...
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ژورنال
عنوان ژورنال: Bulletin of the Geological Society of Finland
سال: 1996
ISSN: 1799-4632,0367-5211
DOI: 10.17741/bgsf/68.1.002