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?

P. Tropper، نويسنده , , I. Deibl، نويسنده , , F. Finger and R. Kaindl ، نويسنده ,

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