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 …

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

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 history of the southern central Andes, including the world's second largest plateau and
adjacent intermontane basins and ranges of the Eastern Cordillera and the northern Sierras …

Simultaneous breakthroughs in our understanding of plate-tectonic processes, depositional
systems, subsidence mechanisms, chronostratigraphy, and basin-exploration methods have …

The early onset of deformation following the India-Asia collision, Neogene expanse of uplift,
and complex systems that comprise strike-slip faults, thrust faults, and intermontane basins …

The Cenozoic Tian Shan is one of the preeminent examples of an intracontinental orogen.
However, there remains a significant controversy over when deformation related to the India …

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 …

The northern part of the Pamir orogen is the preeminent example of an active
intracontinental subduction zone in the early stages of continent–continent collision. Such …

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 …