Slip rate deficit and earthquake potential on shallow megathrusts
Slip rate deficit and earthquake potential on shallow megathrusts
复制标题
浅层巨型逆冲断层的滑移率赤字和地震潜力
DOI:
10.1038/s41561-021-00736-x
复制
发表时间:
2021
影响因子:
18.3
通讯作者:
Lindsey E
中科院分区:
文献类型:
--
作者:
Lindsey E
Most destructive tsunamis are caused by seismic slip on the shallow part of offshore megathrusts. The likelihood of this behaviour is partly determined by the interseismic slip rate deficit, which is often assumed to be low based on frictional studies of shallow fault material. Here, we present a new method for inferring the slip rate deficit from geodetic data that accounts for the stress shadow cast by frictionally locked patches, and show that this approach greatly improves our offshore resolution. We apply this technique to the Cascadia and Japan Trench megathrusts and find that, wherever locked patches are present, the shallow fault generally has a slip rate deficit between 80 and 100% of the plate convergence rate, irrespective of its frictional properties. This finding rules out areas of low kinematic coupling at the trench considered by previous studies. If these areas of the shallow fault can slip seismically, the global tsunami hazard could be higher than currently recognized. Our method identifies critical locations where seafloor observations could yield information about frictional properties of these faults so as to better understand their slip behaviour.
登录
查看更多内容
影响因子:
3.5
作者:
Wessel, P.;Luis, J. F.;Tian, D.
通讯作者:
Tian, D.
影响因子:
--
作者:
C. Scholz;J. Campos
通讯作者:
C. Scholz;J. Campos
影响因子:
--
作者:
R. Kanda;M. Simons
通讯作者:
M. Simons
影响因子:
3.9
作者:
Herman, Matthew W.;Furlong, Kevin P.;Govers, Rob
通讯作者:
Govers, Rob
影响因子:
2
作者:
Metois, M.;Vigny, C.;Socquet, A.
通讯作者:
Socquet, A.