The Trans-Mexican Volcanic Belt (TMVB) is a 1000km long Neogene continental arc
showing a large variation in composition and volcanic style, and an intra-arc extensional …

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

The cause of the Laramide phase of mountain building remains uncertain. Conceptual
models implicate the subduction of either ocean ridges or conjugates of the buoyant Hess or …

Integrated magmatic, structural, and geophysical data provide a basis for modeling the
Neogene lithospheric evolution of the high Central Andean Puna-Altiplano Plateau …

Much progress has been made over the past several decades in delineating the structure of
subducting slabs, but several key aspects of their dynamics remain poorly constrained …

Based on analysis of data from a trans‐Mexico temporary broadband seismic network
centered on Mexico City, we report that the subducting Cocos Plate beneath central Mexico …

Subducting plates around the globe display a large variability in terms of slab geometry,
including regions where smooth and little variation in subduction parameters is observed …

How flat slab geometries are generated has been long debated. It has been suggested that
trenchward motion of thick cratons in some areas of South America and Cenozoic North …

Abstract The East Kunlun Orogen is an integral component of the northern Qinghai-Tibet
plateau. Here we synthesize the geologic, geochemical, geochronological and …

High wavespeed tomographic anomalies shallower than 1100km beneath the India/Asia
collision zone are interpreted as continental slabs subducted during collision. Combining …