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 …

Since the advent of plate tectonics different global reference frames have been used to
describe the motion of plates and trenches. The difference in plate motion and trench …

La extraordinaria diversidad magmática de la Faja Volcánica Transmexicana está
controlada (directa o indirectamente) por dos placas oceánicas independientes cuyos …

Flat or near-horizontal subduction of oceanic lithosphere has been an important tectonic
process both currently and in the geologic past. Subduction of the aseismic Nazca Ridge …

East Asia is a region of widespread deformation, dominated by normal and strike-slip faults.
Deformation has been interpreted to result from extrusion tectonics related to the India …

The subduction-related Michoacán–Guanajuato Volcanic Field (MGVF) in central Mexico
contains∼ 900 cinder cones and numerous larger shield volcanoes of Late Pliocene to …

We combine velocities for 14 continuous GPS stations spanning Mexico and 173 additional
continuous GPS sites on the North American and Pacific plates to study the large‐scale …

Interactions between volcanic and tectonic processes affect the distribution, morphology,
and volume of eruptive products in space and time. The Queréndaro area in the eastern …

The evolution of the continental intraarc Taupo Rift in the North Island, New Zealand, is
rapid, significantly faster than comparative intracontinental rifts such as the African Rifts …

El sistema de fallas Morelia–Acambay (MAFS) consiste en una serie de fallas normales de
dirección E–W y NE–SW que cortan la parte central del Cinturón Volcánico Transmexicano …