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
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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
Heesemann, Martin
中科院分区:
地球科学1区
文献类型:
--
作者:
McGuire, Jeffrey J.;Collins, John A.;Davis, Earl;Becker, Keir;Heesemann, Martin

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俯冲带大地震在逆冲断层破裂的上倾程度上变化很大。由于海底监测的俯冲带数量有限,目前尚不清楚这种多样性是否反映了震间应变累积的变化。我们使用一个钻孔地震大地观测台安装在卡斯卡迪亚断层的上倾端离岸温哥华岛,显示那里的巨型逆冲断层似乎没有滑动触发震颤或慢滑事件时,受到中等动态应力瞬变。最近发生的地震M7.6 -8.1的钻孔倾斜和地震数据表明,尽管1-10 kPa的剪应力瞬变足以触发界面下倾端的震颤,但在Mw4.0级以上没有触发的缓慢滑动,也没有触发的震颤。我们的观测结果与一个模型最为一致,在该模型中,温哥华岛近海的卡斯卡迪亚断层一直锁定到海沟。
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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