As the archetype of mountain building in subduction zones, the Central Andes has
constituted an excellent example for investigating mountain-building processes for decades …

Abstract The Andean hinterland of Chile and Argentina defines a region of voluminous
magmatism, polyphase deformation, and high topography above a long-lived subduction …

The Iglesia basin hosts a key sedimentary archive of the evolution of the southern Central
Andes. This basin is classically interpreted as recording the transition from an outer-to an …

Understanding the effects of flat slab subduction on mountain building, arc magmatism, and
basin evolution is fundamental to convergent‐margin tectonics, with implications for …

The Andes between 28° and 30° S represent a transition between the Puna‐Altiplano
Plateau and the Frontal/Principal Cordillera fold‐and‐thrust belts to the south. While …

ARAMENDIA, Inés; CUITINO, José I; GHIGLIONE, Matías y BOUZA, Pablo José.
Tectonostratigraphic significance of the neogene sedimentary record of northwestern Austral …

Abstract The Southern Puna (∼ 24° S to 27° S) is an outstanding segment of the Central
Andes where the subduction of aseismic ridges, multi-scale lithospheric foundering, and the …

Abstract The southern Central Andes recorded retroarc shortening, basin evolution, and
magmatic arc migration during Neogene changes in subduction. At 31–33° S, above the …

Retroarc foreland basins in contractional arc settings contain evidence of temporal and
spatial variations in magmatic activity, deformation, and exhumation along the continental …

We assess the role of inherited structures on the Meso‐Cenozoic tectonic evolution of the
main Andean Cordillera in central Chile (33° 30′ S‐34° S). Based on extensive field …