The removal, redistribution, and transient storage of sediments in tectonically active
mountain belts is thought to exert a first-order control on shallow crustal stresses, fault …

The northwest Argentine Andes constitute a premier natural laboratory to assess the
complex interactions between isolated uplifts, orographic precipitation gradients, and related …

Abstract The thick-skinned Sierras Pampeanas morphotectonic domain of western and
northwestern Argentina (27° S–33° S) is characterized by reverse-fault–bounded basement …

The Choromoro Basin, an intramontane structural depression in the foreland fold-and-thrust
belt of the central Andes of northwestern Argentina, is underlain by Proterozoic–Recent …

The style and mechanisms by which a foreland region is incorporated into an orogen
depends on the tectonic style, effectiveness of uplift, and dynamic subsidence. Classical …

The study area is located within the Central Andes, a complex region composed of different
structural styles. The region is characterized by highly elevated basement cored ranges …

Abstract A> 15-20 km-thick succession in southern Bolivia forms the most-complete
stratigraphic record in western Gondwana. Upper Neoproterozoic–Carboniferous clastic …

Unravelling the spatiotemporal evolution of the Cenozoic Andean (Altiplano‐Puna) plateau
has been one of the most intriguing problems of South American geology. Despite a number …

Foreland basins are sensitive recorders of spatiotemporal variations in tectonic and climatic
forcing associated with an approaching orogenic front. Thus, analysis of foreland deposits …

Abstract The Central Andes are the product of contractional deformation related to
subduction of the Nazca plate beneath the South American continent. In this geodynamic …