GNGTS 2016 - Atti del 35° Convegno Nazionale

GNGTS 2016 S essione 1.2 243 and with contact metamorphism assemblages replacing greenschist facies assemblages. The computed extent of the aureole for the simulations is wider than the mapped one because the computed thermal boundary of the aureole is between 300 and 400°C. Finally, the thermal gradient of the country rocks at the time of pluton intrusion is sufficiently high to justify the emplacement of Biella pluton during the accomplishment of the break-off of the Alpine slab. References Babist J., Handy M. R., Konrad-Schmolke M., Hammerschmidt K.; 2006: Precollisional, multistage exhumation of subducted continental crust: The Sesia Zone, western Alps. Tectonics, 25 , TC6008, doi: 10.1029/2005TC001927. Bartoli O., Meli S., Sassi R., Magaraci D.; 2013: Amphiboles and clinopyroxenes from Euganean (NE Italy) cumulus enclaves: evidence of subduction-related melts below Adria microplate. Rend Lincei, 24 , 151–���� ���� �������� 161, doi: 10.1007/ s12210-013-0232-6. 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