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Transpressional deformation in northwestern Sardinia (Italy): insights on the tectonic evolution of the Variscan Belt

Carosi, Rodolfo and Oggiano, Giacomo (2002) Transpressional deformation in northwestern Sardinia (Italy): insights on the tectonic evolution of the Variscan Belt. Comptes rendus. Geosciences, Vol. 334 (4), p. 287-294. ISSN 1631-0713. Article.

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DOI: 10.1016/S1631-0713(02)01740-6


Structural investigations in northwestern Sardinia highlight the occurrence of a regional D2 transpressional deformation related both to NNE–SSW direction of compression and to a NW–SE shear displacement. The deformation is continuous and heterogeneous, showing a northward strain increase, indicated by progressively tighter folds and occurrence of F2 sheath folds. D2 transpression is characterised by the presence of a crustal-scale shear deformation overprinting previous D1 structures, related to nappe stacking and top-to-the-south and southwest thrusting. The L2 prominent stretching lineation points to an orogen-parallel extension and to a change in the tectonic transport from D1 to D2. It is attributed to the position of Sardinia close to the northeastern part of the Cantabrian indenter during the progressive evolution of the Ibero-Armorican Arc. D1 phase developed during initial frontal collision, whereas D2 deformation characterised the progressive effect of horizontal displacement during the increasing curvature of the arc.

Item Type:Article
ID Code:5275
Uncontrolled Keywords:Tectonics, transpression, Variscan Belt, folds, stretching lineations, Sardinia
Subjects:Area 04 - Scienze della terra > GEO/03 Geologia strutturale
Divisions:001 Università di Sassari > 01 Dipartimenti > Scienze botaniche, ecologiche e geologiche
Copyright Holders:© 2002 Académie des sciences/Éditions scientifiques et médicales Elsevier SAS
Deposited On:21 Dec 2010 12:49

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