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Cascadia subduction tremor muted by crustal faults

GEOLOGY, no. 6 (2017): 515-518

Cited by: 13|Views2
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Abstract

Deep, episodic slow slip on the Cascadia subduction megathrust of western North America is accompanied by low-frequency tremor in a zone of high fluid pressure between 30 and 40 km depth. Tremor density (tremor epicenters per square kilometer) varies along strike, and lower tremor density statistically correlates with upper plate faults t...More

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