Geology of the Susa Shear Zone (Susa Valley, Western Alps)

The 1:10,000 scale geological map of the Susa Shear Zone (SSZ) in the inner sector of the Western Alps, aims to describe the geological setting and tectonic evolution of a first-order Alpine shear zone, which drove exhumation and juxtaposition of different oceanic and continental margin units (i.e....

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Main Authors: Stefano Ghignone, Marco Gattiglio, Gianni Balestro, Alessandro Borghi
Format: Article
Language:English
Published: Taylor & Francis Group 2020-12-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2019.1698473
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spelling doaj-2a8ec0600a4d4ead94545b672db1a2ff2021-01-15T13:32:55ZengTaylor & Francis GroupJournal of Maps1744-56472020-12-01162798610.1080/17445647.2019.16984731698473Geology of the Susa Shear Zone (Susa Valley, Western Alps)Stefano Ghignone0Marco Gattiglio1Gianni Balestro2Alessandro Borghi3Department of Earth Sciences, University of TorinoDepartment of Earth Sciences, University of TorinoDepartment of Earth Sciences, University of TorinoDepartment of Earth Sciences, University of TorinoThe 1:10,000 scale geological map of the Susa Shear Zone (SSZ) in the inner sector of the Western Alps, aims to describe the geological setting and tectonic evolution of a first-order Alpine shear zone, which drove exhumation and juxtaposition of different oceanic and continental margin units (i.e. the blueschist-facies External Piedmont Zone in its hanging wall and the eclogite-facies Internal Piedmont Zone and Dora Maira Massif in its footwall). The SSZ corresponds to a tectonic mélange showing a block-in-matrix structure, wherein mylonitic calcschists embed blocks of different rock units. Geological mapping and structural analysis investigated overprinting relationships among shear planes and structures related to different deformation phases: they show that the SSZ evolved through two tectonic events, during which apparent reverse top-to-E shear planes were superposed by extensional top-to-W ones.http://dx.doi.org/10.1080/17445647.2019.1698473western alpine ophiolitestectonic mélangesorogenic exhumation processespolyphase shear zones
collection DOAJ
language English
format Article
sources DOAJ
author Stefano Ghignone
Marco Gattiglio
Gianni Balestro
Alessandro Borghi
spellingShingle Stefano Ghignone
Marco Gattiglio
Gianni Balestro
Alessandro Borghi
Geology of the Susa Shear Zone (Susa Valley, Western Alps)
Journal of Maps
western alpine ophiolites
tectonic mélanges
orogenic exhumation processes
polyphase shear zones
author_facet Stefano Ghignone
Marco Gattiglio
Gianni Balestro
Alessandro Borghi
author_sort Stefano Ghignone
title Geology of the Susa Shear Zone (Susa Valley, Western Alps)
title_short Geology of the Susa Shear Zone (Susa Valley, Western Alps)
title_full Geology of the Susa Shear Zone (Susa Valley, Western Alps)
title_fullStr Geology of the Susa Shear Zone (Susa Valley, Western Alps)
title_full_unstemmed Geology of the Susa Shear Zone (Susa Valley, Western Alps)
title_sort geology of the susa shear zone (susa valley, western alps)
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2020-12-01
description The 1:10,000 scale geological map of the Susa Shear Zone (SSZ) in the inner sector of the Western Alps, aims to describe the geological setting and tectonic evolution of a first-order Alpine shear zone, which drove exhumation and juxtaposition of different oceanic and continental margin units (i.e. the blueschist-facies External Piedmont Zone in its hanging wall and the eclogite-facies Internal Piedmont Zone and Dora Maira Massif in its footwall). The SSZ corresponds to a tectonic mélange showing a block-in-matrix structure, wherein mylonitic calcschists embed blocks of different rock units. Geological mapping and structural analysis investigated overprinting relationships among shear planes and structures related to different deformation phases: they show that the SSZ evolved through two tectonic events, during which apparent reverse top-to-E shear planes were superposed by extensional top-to-W ones.
topic western alpine ophiolites
tectonic mélanges
orogenic exhumation processes
polyphase shear zones
url http://dx.doi.org/10.1080/17445647.2019.1698473
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