Hirono Tetsuro, Tsuda Kenichi, Tanikawa Wataru, Ampuero Jean-Paul, Shibazaki Bunichiro, Kinoshita Masataka, Mori James J
Department of Earth and Space Science, Graduate School of Science, Osaka University, Toyonaka, Osaka 560-0043, Japan.
Center for Safety and Reliability Engineering, Institute of Technology Shimizu Corporation, Koto, Tokyo 135-8530, Japan.
Sci Rep. 2016 Jun 20;6:28184. doi: 10.1038/srep28184.
Near-trench slip during large megathrust earthquakes (megaquakes) is an important factor in the generation of destructive tsunamis. We proposed a new approach to assessing the near-trench slip potential quantitatively by integrating laboratory-derived properties of fault materials and simulations of fault weakening and rupture propagation. Although the permeability of the sandy Nankai Trough materials are higher than that of the clayey materials from the Japan Trench, dynamic weakening by thermally pressurized fluid is greater at the Nankai Trough owing to higher friction, although initially overpressured fluid at the Nankai Trough restrains the fault weakening. Dynamic rupture simulations reproduced the large slip near the trench observed in the 2011 Tohoku-oki earthquake and predicted the possibility of a large slip of over 30 m for the impending megaquake at the Nankai Trough. Our integrative approach is applicable globally to subduction zones as a novel tool for the prediction of extreme tsunami-producing near-trench slip.
大型逆冲型地震(巨震)期间的海沟附近滑动是产生破坏性海啸的一个重要因素。我们提出了一种新方法,通过整合实验室得出的断层物质属性以及断层弱化和破裂扩展模拟,来定量评估海沟附近的滑动潜力。尽管南海海槽含沙物质的渗透率高于日本海沟的黏土物质,但由于摩擦力较高,南海海槽内热压流体引起的动态弱化作用更强,不过南海海槽最初的超压流体抑制了断层弱化。动态破裂模拟再现了2011年东北冲地震中在海沟附近观测到的大滑动,并预测了南海海槽即将发生的巨震有超过30米的大滑动可能性。我们的综合方法作为预测产生极端海啸的海沟附近滑动的一种新工具,可全球应用于俯冲带。