Mesozoic Cenozoic evolution of the Southern Patagonian Andes fold and thrust belt (47-48S): Influence of the Rocas Verdes basin inversion and onset of Patagonian glaciations

GHIGLIONE, MATÍAS C.; TOBAL, JONATHAN; BARBERÓN, VANESA; RONDA, GONZALO; COUTAND, ISABELLE

TECTONOPHYSICS

ELSEVIER SCIENCE BV

Año: 2019 vol. 765 p. 83 - 101

0040-1951

The Southern Patagonian Andes (SPA)between 47°?48°S are characterized by relatively high elevations (1500?4000 m)and a 200-km-wide, largely exhumed, basement domain along the backbone of the Cordillera, bounded by a narrow 30-km-wide fold and thrust-belt to the east. The tectonic evolution of the SPA includes widespread Jurassic extension during the opening of the Austral-Magallanes basin and the Rocas Verdes back-arc oceanic basin (RVB), followed by Cretaceous to Cenozoic shortening. Although the main phases of deformation that affected this Andean segment have been the focus of previous studies, its finite geometry and step by step structural and kinematic evolution have not been quantitatively determined. In this work, we present kinematically restored cross sections, showing the variable geometry, trough time, of the eastern basement domain and the fold and thrust-belt. A regional westward-dipping listric decollement, interpreted as formed during the Jurassic extensional event, was reactivated during the Andean deformation constituting the main detachment surface of basement structures and the fold and thrust belt. West verging faults systems are considered a consequence of inversion of north-south trending extensional features as passive roof high-angle west-vergent faults. Using regional data such as field relations, unconformities, and existing ages to differentiate deformational stages, three main phases of contractional deformation are proposed for the area, starting with an Aptian - Cenomanian? phase related to inversion of the extensional depocenter in inmediate response to the closure of northernmost RVB. A second, Miocene phase responsible for most of the shortening occurred between 18 Ma and 10 Ma. Finally, the onset of glaciations and glacial erosion might have triggered out-of-sequence thrusting in the interior of the orogen after 7 Ma.