Understanding Slow Slip and Tremor on Plate Boundaries

Unlocking the secrets of episodic slow slip and tremor

Episodic tremor and slip on the Cascadia subduction zone: the chatter of silent slip.

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 nonearthquake seismic signatures. Tremorlike seismic signals were found to correlate temporally and spatially with slip events identified from crustal motion data spanning the past 6 years. During the period between slips, tremo...

On the application of slip boundary condition on curved boundaries

Hydrodynamic simulations of sloshing phenomena often involve the application of slip boundary condition at the wetted surfaces. If these surfaces are curved, the ambiguous nature of the normal vector in the discretized problem can interfere with the application of such a boundary condition. Even the use of consistent normal vectors, preferred from the point of view of conservation, does not ass...

Tremors and Slow Slip Events Slow Earthquakes Coincident with Episodic

www.sciencemag.org (this information is current as of February 2, 2007 ): The following resources related to this article are available online at http://www.sciencemag.org/cgi/content/full/315/5811/503 version of this article at: including high-resolution figures, can be found in the online Updated information and services, http://www.sciencemag.org/cgi/content/full/1134454/DC1 can be found at:...

Seismic and geodetic constraints on Cascadia slow slip

[1] Automatically detected and located tremor epicenters from episodic tremor and slip (ETS) episodes in northern Cascadia provide a high-resolution map of Washington’s slow slip region. Thousands of epicenters from the past four ETS events from 2004 to 2008 provide detailed map-view constraints that correlate with geodetic estimates of the simultaneous slow slip. Each of these ETS events exhib...