Articles | Volume 12, issue 8
https://doi.org/10.5194/se-12-1967-2021
https://doi.org/10.5194/se-12-1967-2021
Research article
 | 
26 Aug 2021
Research article |  | 26 Aug 2021

Geodynamic and seismotectonic model of a long-lived transverse structure: The Schio-Vicenza Fault System (NE Italy)

Dario Zampieri, Paola Vannoli, and Pierfrancesco Burrato

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Latest update: 13 Dec 2024
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Short summary
The long-lived Schio-Vicenza Fault System is a major shear zone cross-cutting the foreland and the thrust belt of the eastern southern Alps. We review 150 years of scientific works and explain its activity and kinematics, characterized by sinistral and dextral transcurrent motion along its southern and northern sections, respectively, by a geodynamic model that has the Adria indenter as the main actor and coherently reconciles the available geological and geophysical evidence collected so far.