Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Law R.D.[4]"'
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f74f093791ee2cd8c8b5e9755122e5ca
https://publications.cnr.it/doc/455995
https://publications.cnr.it/doc/455995
Publikováno v:
Tectonics (Online) 39 (2020). doi:10.1029/2020TC006153
info:cnr-pdr/source/autori:Simonetti M.[1], Carosi R.[1], Montomoli C.[1,2], Cottle J.M.[3], Law R.D.[4]/titolo:Transpressive Deformation in the Southern European Variscan Belt: New Insights From the Aiguilles Rouges Massif (Western Alps)/doi:10.1029%2F2020TC006153/rivista:Tectonics (Online)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:39
info:cnr-pdr/source/autori:Simonetti M.[1], Carosi R.[1], Montomoli C.[1,2], Cottle J.M.[3], Law R.D.[4]/titolo:Transpressive Deformation in the Southern European Variscan Belt: New Insights From the Aiguilles Rouges Massif (Western Alps)/doi:10.1029%2F2020TC006153/rivista:Tectonics (Online)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:39
Despite the Mediterranean sector of the Variscan Belt being fragmented and reworked during Alpine orogenesis, evidence for the activity of a right-lateral strike-slip shear zone has been reported in Paleozoic fragments of the belt such as the Sardini
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::33a9aad6210c2ea411991a698c1e2cd2
http://hdl.handle.net/2318/1755378
http://hdl.handle.net/2318/1755378