Short-and long-term processes at or close to the subduction plate interface (eg, mineral
transformations, fluid release, seismicity and more generally deformation) might be more …

Geodesy, the oldest science, has become an important discipline in the geosciences, in
large part by enhancing Global Positioning System (GPS) capabilities over the last 35 years …

Modern geodetic and seismologic observations describe the behavior of fault slip over a
vast range of spatial and temporal scales. Slip at sub-seismogenic speeds is evident from …

The existence of an observable precursory phase of slip on the fault before large
earthquakes has been debated for decades. Although observations preceding several large …

The range of fault slip behaviors near the trench at subduction plate boundaries is critical to
know, as this is where the world's largest, most damaging tsunamis are generated. Our …

This essential reference for graduate students and researchers provides a unified treatment
of earthquakes and faulting as two aspects of brittle tectonics at different timescales. The …

We document geodetic strain across the Nepal Himalaya using GPS times series from 30
stations in Nepal and southern Tibet, in addition to previously published campaign GPS …

The discovery of slow-slip phenomena has revolutionized our understanding of how faults
accommodate relative plate motions. Faults were previously thought to relieve stress either …

Earthquakes occur mainly on active faults. Fault slip is closely related to seismicity and is
thus widely discussed in Geosciences, Seismology, and Engineering. Slip experiment is a …

Understanding the partitioning of seismic and aseismic fault slip is central to seismotectonics
as it ultimately determines the seismic potential of faults. Thanks to advances in tectonic …