La ricostruzione dei percorsi P-T nei ciottoli dei conglomerati Permiani delle Alpi Meridionali come chiave d’interpretazione geodinamica

The reconstruction of P-T path in metamorphic pebbles of Southalpine Permian conglomerates (Dosso dei Galli Conglomerate = DGC, Monte Aga and Val Vedello conglomerates = AVC and Ponteranica Formation = PF) and the comparison of the results with the P-T-d-t paths of basement tectono-mertamorphic units suggest that the exhumation age of the Southalpine deep crust rejuvenates westward and that a migration from East to West, of the tectonic regime triggering basins opening, occurred.