Deep earthquakes behave like shallow earthquakes but must have fundamentally different
physical processes. Their rupture behaviors, magnitude-frequency statistics, and aftershocks …

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 …

We present a novel method for joint inversion of receiver functions and surface wave
dispersion data, using a transdimensional Bayesian formulation. This class of algorithm …

Water and hydrous minerals play a key part in geodynamic processes at subduction zones,,
by weakening the plate boundary, aiding slip and permitting subduction—and indeed plate …

A non-linear Bayesian Monte-Carlo method is presented to estimate a Vsv model beneath
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …

A new model of the subducted Juan de Fuca plate beneath western North America allows
first‐order correlations between the occurrence of Wadati‐Benioff zone earthquakes and …

In the Cascadia subduction zone, beneath southern Vancouver Island at 25–45 km depth,
converted teleseismic waves reveal an∼ 5-km-thick landward-dip** layer with …

We find that in young and warm subducting plates, earthquakes occur just below the Moho.
In older plates, earthquakes occur throughout the subducting oceanic crust, as well as the …

We employ 130 low‐frequency earthquake (LFE) templates representing tremor sources on
the plate boundary below southern Vancouver Island to examine LFE magnitudes. Each …

An ensemble‐averaging technique is used to remove the long‐wavelength topography and
gravity field associated with subduction zones. Short‐wavelength residual anomalies are …