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What’s down there? The structures, materials and environment of deep-seated slow slip and tremor

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By Whitney Behr, Roland Burgmann, Behr Whitney M, Bürgmann Roland
| royalsocietypublishing.org
1. Introduction What was long considered to be bothersome seismic noise and long-period errors in geodetic time series turned out to be one of the exciting discoveries in the Earth Sciences in recent decades: episodic slow slip events (SSEs) and associated tremor signals originating deep on the plate interface of the Nankai, Japan, and Cascadia, Canada and USA, subduction zones (figure 1) [1–3].
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