Deep-seated slow slip and tremor (SST), including slow slip events, episodic tremor and
slip, and low-frequency earthquakes, occur downdip of the seismogenic zone of numerous …

Continuously operating global positioning system sites in the North Island of New Zealand
have revealed a diverse range of slow motion earthquakes on the Hikurangi subduction …

Many types of hydrothermal ore deposits form at overpressured conditions during high fluid
flux through fault zones in the continental seismogenic regime. These include many …

The recognition of slow earthquakes in geodetic and seismological data has transformed the
understanding of how plate motions are accommodated at major plate boundaries. Slow …

Slow fault slip includes a range of transient phenomena that occur over timescales longer
than those of standard earthquakes. Slow slip events are often closely associated with …

Episodic tremor and accompanying slow slip are observed at the down-dip edge of
subduction seismogenic zones. While tremors are the seismic signature of this …

Continental transform faults are dominantly highly localized strike-slip shear zones
hundreds of kilometers long that accumulate tens to hundreds of kilometers of displacement …

In this study we first summarize the constraints that on the Cascadia subduction thrust, there
is a 70 km gap downdip between the megathrust seismogenic zone and the Episodic …

At many plate boundaries, conditions in the transition zone between seismogenic and stable
slip produce slow earthquakes. In the Cascadia subduction zone, these events are …

The recurrence patterns of the Parkfield tremors with period‐multiplying slow and fast
ruptures provide new insights on the physics of earthquake cycles. However, the …