Slow earthquakes are episodic slow fault slips. They form a fundamental component of
interplate deformation processes, along with fast, regular earthquakes. Recent …

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 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 …

Earthquake and Volcano Deformation is the first textbook to present the mechanical models
of earthquake and volcanic processes, emphasizing earth-surface deformations that can be …

We found that repeated slow slip events observed on the deeper interface of the northern
Cascadia subduction zone, which were at first thought to be silent, have unique …

Apparent seasonal site position variations are derived from 4.5 years of global continuous
GPS time series and are explored through the “peering” approach. Peering is a way to …

Continuous Global Positioning System sites in southwestern British Columbia, Canada, and
northwestern Washington state, USA, have been moving landward as a result of the locked …

Recently, a series of unusual earthquake phenomena have been discovered, including
deep episodic tremor, low-frequency earthquakes, very-low-frequency earthquakes, slow …