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P–T–tevolution 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-Tevents in the Moldanubian Unit?
P. Tropper, I. Deibl, F. Finger, R. KaindlVolume:
95
Language:
english
Pages:
19
DOI:
10.1007/s00531-006-0082-x
Date:
November, 2006
File:
PDF, 1.17 MB
english, 2006