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 …

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 …

Non-volcanic tremor (NVT) and episodic slow slip events (SSEs) have been observed below
the seismogenic zone of relatively warm subduction zones for the past 20 years …

Broken foreland basins are caused by crustal-scale contractional basement structures that
compartmentalize (or break) a contiguous retroarc or collisional foreland basin into smaller …

More than a decade after the discovery of deep episodic slow slip and tremor, or slow
earthquakes, at subduction zones, much research has been carried out to investigate the …

Slow earthquakes are important constituents of the seismic cycle and are involved in the
stress transfer between the viscously slipping portion of the plate interface and the …

Rapid tremor migration (RTM) in subduction zones is a manifestation of complex fault-zone
processes on the plate interface. Recent observations have revealed a large diversity of …

Studies of low‐frequency earthquakes (LFEs) have focused on detecting events within
previously identified tectonic tremor. However, the principal LFE detection tools of matched …

Abstract The Middle America subduction zone (MASZ) is one of the world'most complex
convergent margins as it involves the subduction of the Rivera and Cocos young oceanic …

Slow transient slip that releases stress along the deep roots of plate interfaces is most often
observed on regional GPS networks installed at the surface. The detection of slow slip is not …