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 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 …

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 …

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

In subduction zones, landward dipping regions of low shear wave velocity and elevated
Poisson's ratio, which can extend to at least 120 km depth, are interpreted to be all or part of …

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