Integration of regional stratigraphic relationships with data on sediment accumulation,
provenance, paleodrainage, and deformation timing enables a reconstruction of Mesozoic …

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

Construction of the Andes has been governed largely by fluctuating contractional, neutral,
and extensional tectonic regimes during differing degrees of mechanical coupling along the …

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 temporal transition from backarc extension to retroarc shortening is a fundamental
process in the evolution of many Andean-type convergent margins. This switch in tectonic …

Cooling subvolcanic igneous intrusions are known to have a tremendous impact on fluid
flow in the shallow Earth's crust. However, the long-term post-cooling legacy of subvolcanic …

Cooling subvolcanic igneous intrusions are known to have a substantial impact on fluid flow
in the shallow Earth's crust, for example activation of geothermal systems, circulation of …

A balanced cross-section spanning the Eastern Cordillera and Subandean Zone of southern
Peru (13–15° S) constrains~ 130 km (38%) of Cenozoic orogen-normal SW–NE Andean …

Andean orogenesis is expressed in the diverse deformational records of crustal structures
and sedimentary basins in western South America. Here we summarize retroarc structural …

We assess the role of inherited structures on the Meso‐Cenozoic tectonic evolution of the
main Andean Cordillera in central Chile (33° 30′ S‐34° S). Based on extensive field …