P–T–t evolution of spinel–cordierite–garnet gneisses from the Sauwald Zone (Southern Bohemian Massif, Upper Austria): is there evidence for two independent late-Variscan low-P/high-T events in the Moldanubian Unit?

Author： Tropper P.   Deibl I.   Finger F.   Kaindl R.  

Publisher： Springer Publishing Company

ISSN： 1437-3254

Source： International Journal of Earth Sciences, Vol.95, Iss.6, 2006-11, pp. : 1019-1037

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