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Geodetic and seismic signatures of episodic tremor and slip in the northern Cascadia subduction zone

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Dragert, H., Wang, K., Rogers, G.·2014·Earth, Planets and Space

Abstract

Slip events with an average duration of about 10 days and effective total slip displacements of severalc entimetres have been detected on the deeper (25 to 45 km) part of the northern Cascadia subduction zone interface by observing transient surface deformation on a network of continuously recording Global Positioning System (GPS) sites. The slip events occur down-dip from the currently locked, seismogenic portion of the subduction zone, and, for the geographic region around Victoria, British Columbia, repeat at 13 to 16 month intervals. These episodes of slip are accompanied by distinct, low-frequency tremors, similar to those reported in the forearc region of southern Japan. Although the processes which generate this phenomenon of episodic tremor and slip (ETS) are not well understood, it is possible that the ETS zone may constrain the landward extent of megathrust rupture, and conceivable that an ETS event could precede the next great thrust earthquake.

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Metadata

Authors
Dragert, H., Wang, K., & Rogers, G.
Venue
Earth, Planets and Space
Published
2014-06-26
Volume
56
Issue
12
Pages
1143-1150
ISSN
  • 1343-8832 (ISSN-L)
  • 1880-5981
OpenAlex
W2166482715
Cited by
184
References
1
FWCI
11.60
Type
journal article
Language
en
Open access
gold

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CoChat. (2026). Citation check: Geodetic and seismic signatures of episodic tremor and slip in the northern Cascadia subduction zone. https://app.cochat.ai/papers/10.1186/bf03353333
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Dragert, H., Wang, K., & Rogers, G. (2014). Geodetic and seismic signatures of episodic tremor and slip in the northern Cascadia subduction zone. Earth, Planets and Space. https://doi.org/10.1186/bf03353333

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