A Lack of Dynamic Triggering of Slow Slip and Tremor Indicates That the Shallow Cascadia Megathrust Offshore Vancouver Island Is Likely Locked
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- Jeffrey J. McGuire
- Department of Geology and Geophysics Woods Hole Oceanographic Institution Woods Hole MA USA
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- John A. Collins
- Department of Geology and Geophysics Woods Hole Oceanographic Institution Woods Hole MA USA
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- Earl Davis
- Pacific Geoscience Centre Geological Survey of Canada Sidney British Columbia Canada
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- Keir Becker
- Department of Marine Geosciences University of Miami–RSMAS Miami FL USA
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- Martin Heesemann
- Ocean Networks Canada University of Victoria Victoria British Columbia Canada
書誌事項
- 公開日
- 2018-10-27
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#am
- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1029/2018gl079519
- 公開者
- American Geophysical Union (AGU)
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説明
<jats:title>Abstract</jats:title><jats:p>Great subduction zone earthquakes vary considerably in the updip extent of megathrust rupture. It is unclear if this diversity reflects variations in interseismic strain accumulation owing to the limited number of subduction zones with seafloor monitoring. We use a borehole seismic‐geodetic observatory installed at the updip end of the Cascadia fault offshore Vancouver Island to show that the megathrust there does not appear to slip in triggered tremor or slow‐slip events when subjected to moderate dynamic stress transients. Borehole tilt and seismic data from recent teleseismic <jats:italic>M</jats:italic>7.6–8.1 earthquakes demonstrate a lack of triggered slow slip above the <jats:italic>M</jats:italic><jats:sub><jats:italic>w</jats:italic></jats:sub> 4.0 level and an absence of triggered tremor despite shear‐stress transients of 1–10 kPa that were sufficient to trigger tremor on the downdip end of the interface. Our observations are most consistent with a model in which the Cascadia fault offshore Vancouver Island is locked all the way to the trench.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 45 (20), 1-, 2018-10-27
American Geophysical Union (AGU)
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詳細情報 詳細情報について
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- CRID
- 1363388846043479936
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- ISSN
- 19448007
- 00948276
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- Web Site
- https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2018GL079519
- https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL079519
- https://onlinelibrary.wiley.com/doi/full-xml/10.1029/2018GL079519
- https://agupubs.onlinelibrary.wiley.com/doi/am-pdf/10.1029/2018GL079519
- https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL079519
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