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Publikováno v:
Journal of structural geology 149 (2021): 1–21. doi:10.1016/j.jsg.2021.104399
info:cnr-pdr/source/autori:Simonetti M.[1,2], Carosi R.[2], Montomoli C.[2,3], Law R.D.[4], Cottle J.M.[5]/titolo:Unravelling the development of regional-scale shear zones by a multidisciplinary approach: The case study of the Ferriere-Molli`eres Shear Zone (Argentera Massif, Western Alps)/doi:10.1016%2Fj.jsg.2021.104399/rivista:Journal of structural geology/anno:2021/pagina_da:1/pagina_a:21/intervallo_pagine:1–21/volume:149
info:cnr-pdr/source/autori:Simonetti M.[1,2], Carosi R.[2], Montomoli C.[2,3], Law R.D.[4], Cottle J.M.[5]/titolo:Unravelling the development of regional-scale shear zones by a multidisciplinary approach: The case study of the Ferriere-Molli`eres Shear Zone (Argentera Massif, Western Alps)/doi:10.1016%2Fj.jsg.2021.104399/rivista:Journal of structural geology/anno:2021/pagina_da:1/pagina_a:21/intervallo_pagine:1–21/volume:149
Shear zone behavior is mainly controlled by deformation regime (brittle versus ductile), deformation temperature, strain rate and magnitude, and rheology of the deformed rocks. If a gradient of strain is established across a shear zone, softening phe
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https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f74f093791ee2cd8c8b5e9755122e5ca
https://publications.cnr.it/doc/455995
https://publications.cnr.it/doc/455995