Tectonic tremor: the chatter of mafic underplating beneath southern Vancouver Island?
Geena Littel,
Michael Bostock,
Charles Sammis
et al.
Abstract:Tremor is a low-amplitude seismic signal that usually temporally coincides with episodic slow fault slip at plate boundaries worldwide. Since the discovery of tremor in Cascadia, significant effort has been devoted to understanding its relationship to slow slip. However, its source mechanism has been widely debated, owing in large part to the challenge of locating sources accurately in depth. We assemble a tremor catalog of 4,851 events for a ~ 10 X 20 km2 area on southern Vancouver Island from slow slip episo… Show more
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