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

Cordilleran orogenic systems, such as the modern Andes, are long belts of deformation and
magmatism that are associated with the subduction of oceanic plates beneath continental …

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

Accretionary orogens form at intraoceanic and continental margin convergent plate
boundaries. They include the supra-subduction zone forearc, magmatic arc and back-arc …

Arc-basaltic melts of typical hydration state (≥ 2 wt% H 2 O) are buoyant relative to all
common crustal igneous rock types and may pass adiabatically from a mantle source …

Abstract The Tarim Craton, located in the center of Asia, was involved in the assembly and
breakup of the Rodinia supercontinent during the Neoproterozoic and the subduction …

The four‐part districting scheme (wedge‐top, foredeep, forebulge, and backbulge
depozones) applies to many foreland basin systems worldwide, but significant variations …

The analyses of the main parameters controlling the present Chile‐type and Marianas‐type
tectonic settings developed along the eastern Pacific region show four different tectonic …

The well-known southwest-to-northeast younging of stratigraphy over a present-day cross
strike distance of> 1500 km in the southern Tasmanides of eastern Australia has been used …

Reconfigurations of magmatic arcs through time have been recognized since pioneering
works, describing inland and trenchward arc migrations or magmatic shut-off lasting for …