Detrital thermochronology studies based on the lag-time approach are increasingly
employed to investigate the erosional evolution of mountain belts and perform paleotectonic …

Unconformities in foreland basins may be generated by tectonic processes that operate in
the basin, the adjacent fold–thrust belt or the broader convergent margin. Foreland basin …

The Andes are the culmination of shortening and crustal thickening that commenced during
Late Cretaceous time. First-order questions regarding the tectonic evolution of the central …

In recent decades, the growing interest in wetlands highlights the fundamental role of these
complex ecosystems. Integrated sedimentological and geochemical studies that refer to …

Abstract The Andean Plateau of north‐western Argentina (Puna) at a mean elevation of ca.
4.2 km constitutes the southern continuation of the Altiplano; it is a compressional basin‐and …

Abstract The Sub-Andean retroarc region is a unique example of an active continental-scale
retroarc foreland basin system. Heavily targeted for hydrocarbon exploration, the region …

The rate of channel incision in bedrock rivers is often described using a power law
relationship that scales erosion with drainage area. However, erosion in landscapes that …

It has long been hypothesized that climate can modify both the pattern and magnitude of
erosion in mountainous landscapes, thereby controlling morphology, rates of deformation …

Abstract Within the Central Andes of NW Argentina, the spatiotemporal distribution and style
of deformation is strongly influenced by pre‐Cenozoic heterogeneities, mostly related to the …

Reconstruction of the Cretaceous tectonic evolution of the eastern margin of the Tibetan
Plateau is of great significance to understanding the formation and early evolution of the …