Broken foreland basins are caused by crustal-scale contractional basement structures that
compartmentalize (or break) a contiguous retroarc or collisional foreland basin into smaller …

We here review in terms of tectono-magmatic setting and Quaternary landscape dynamics
what is known about the provenance of Argentine dune fields and their fluvial feeder …

The spatial and temporal distribution of arc magmatism and associated isotopic variations
provide insights into the Phanerozoic history of the western margin of South America during …

The Manantiales basin contains> 4 km of nonmarine sedimentary strata that accumulated at
31.75–32.5° S during construction of the High Andes. We report field and analytical data …

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

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 …

Abstract Central Argentina from the Pampean flat‐slab segment to northern Patagonia (27°–
41° S) represents a classic example of a broken retroarc basin with strong tectonic and …

The Eocene compressional phase is well known to have contributed to the construction of
the Andes orogen at latitudes north of 30° S, but its extension to the south has not been fully …

Abstract Late Oligocene-early Miocene aridification in the retroarc foreland basin adjacent to
the southern central Andes was recorded by widespread eolian conditions that coincided …

Along the western slope of the Central Andes in the southernmost part of the Pampean flat-
slab subduction zone segment (∼ 33° S), crustal Quaternary west-vergent reverse faults are …