A Lack of Dynamic Triggering of Slow Slip and Tremor Indicates That the Shallow Cascadia Megathrust Offshore Vancouver Island Is Likely Locked
A Lack of Dynamic Triggering of Slow Slip and Tremor Indicates That the Shallow Cascadia Megathrust Offshore Vancouver Island Is Likely Locked
复制标题
缺乏慢滑和震颤的动态触发表明温哥华岛近海的卡斯卡迪亚浅层巨型逆冲断层很可能被锁定
DOI:
10.1029/2018gl079519
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发表时间:
2018
影响因子:
5.2
通讯作者:
Heesemann, Martin
中科院分区:
文献类型:
--
作者:
McGuire, Jeffrey J.;Collins, John A.;Davis, Earl;Becker, Keir;Heesemann, Martin
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 teleseismicM7.6–8.1 earthquakes demonstrate a lack of triggered slow slip above theMw4.0 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.
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DOI:
10.5047/eps.2012.04.010
发表时间:
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期刊:
Earth, Planets and Space
影响因子:
--
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1985
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DOI:
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发表时间:
2010
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