Tectono-metamorphic evolution of a post-variscan mid-crustal shear zone in relation to the Tethyan rifting (Ivrea-Verbano Zone, Southern Alps)

Author:

Simonetti M.ORCID,Langone A.ORCID,Bonazzi M.,Corvò S.ORCID,Maino M.ORCID

Publisher

Elsevier BV

Subject

Geology

Reference139 articles.

1. Local disequilibrium of plagioclase in high-temperature shear zones of the Ivrea Zone. Italy;Altenberger;J. Metam. Geol.,1995

2. Evolution of a passive crustal-scale detachment (Syros, Aegean region): insights from structural and petrofabric analyses in the hanging-wall;Aravadinou;J. Struct. Geol.,2017

3. Rheological properties of the mantle lid beneath the Mojave region in southern California;Behr;Earth Planet Sci. Lett.,2014

4. A crustal‐scale view at rift localization along the fossil Adriatic margin of the Alpine Tethys preserved in NW Italy;Beltrando;Tectonics,2015

5. Evolution of mantle melts intruding the lowermost continental crust: constraints from the Monte Capio–Alpe Cevia mafic–ultramafic sequences (Ivrea–Verbano Zone, northern Italy);Berno;Contrib. Mineral. Petrol.,2019

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