In this work, we present the geological map of the San Pellegrino pass, inserted in the spectacular scenario of the Dolomiti region (Southern Alps, Italy), at a scale of 1:10.000 and accompanied by geological cross-sections. The detailed distinction of lithological thin units allowed to achieve a consistent interpretation of the local structural setting by drawing brittle and ductile Alpine tectonic deformations. The differential deformation and structural styles within the geological map are the result of the different rheological nature of volcanic and sedimentary rocks, as well as of the superimposition of compressional Alpine tectonics over Permo-Mesozoic extensional tectonic phases, and consequent reactivation of inherited structures.

Pre-Alpine and Alpine deformation at San Pellegrino pass (Dolomites, Italy)

Abbà, Tiziano
Data Curation
;
Breda, Anna
Investigation
;
Massironi, Matteo
Investigation
;
Preto, Nereo
Investigation
;
Bondesan, Aldino
Investigation
;
Carton, Alberto
Investigation
;
Fontana, Alessandro
Investigation
;
Mozzi, Paolo
Investigation
;
Surian, Nicola
Investigation
;
Zanoner, Thomas
Investigation
;
Zampieri, Dario
Writing – Original Draft Preparation
2018

Abstract

In this work, we present the geological map of the San Pellegrino pass, inserted in the spectacular scenario of the Dolomiti region (Southern Alps, Italy), at a scale of 1:10.000 and accompanied by geological cross-sections. The detailed distinction of lithological thin units allowed to achieve a consistent interpretation of the local structural setting by drawing brittle and ductile Alpine tectonic deformations. The differential deformation and structural styles within the geological map are the result of the different rheological nature of volcanic and sedimentary rocks, as well as of the superimposition of compressional Alpine tectonics over Permo-Mesozoic extensional tectonic phases, and consequent reactivation of inherited structures.
2018
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11577/3284080
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