Mountain building in the Andes, the longest continental mountain range on Earth, started in
the Late Cretaceous but was highly diachronous. Reconstructing the timing of surface uplift …

The largest tectonic relief breaking the Earth's surface (13 km vertically) is at the subduction
margin of the Andes, which generates routinely megathrust earthquakes (Mw> 8.5) and …

Defining the structural style of fold–thrust belts and understanding the controlling factors are
necessary steps towards prediction of their long-term and short-term dynamics, including …

The tectonic and climatic boundary conditions of the broken foreland and the orogen interior
of the southern Central Andes of northwestern Argentina cause strong contrasts in elevation …

Cenozoic strata in the central Andes of northwestern Argentina record the development and
migration of a regional foreland basin system analogous to the modern Chaco‐Paraná …

Quantitative geomorphic research depends on accurate topographic data often collected via
remote sensing. Lidar, and photogrammetric methods like structure-from-motion, provide the …

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

The intraplate fault-block mountains and intermontane deposits of the Gastre Basin, which
are recorded more than 550 km east of the Andean trench in central Patagonia, Argentina …

Fluvial fill terraces in intermontane basins are valuable geomorphic archives that can record
tectonically and/or climatically driven changes of the Earth-surface process system …

Abstract The Central Andes between 18° S and 36° S latitude strike north-south for 2000 km
along the Chilean subduction margin, cross several climate zones from hyperarid to humid …