JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

S (Solid Earth Sciences) » S-SS Seismology

[S-SS08] [EE] Earthquake Modeling and Simulation

Mon. May 22, 2017 3:30 PM - 5:00 PM A02 (Tokyo Bay Makuhari Hall)

convener:Eiichi Fukuyama(National Research Institute for Earth Science and Disaster Prevention), John B Rundle(University of California Davis), Yukitoshi Fukahata(Disaster Prevention Research Institute, Kyoto University), Chairperson:Takashi Furumura(Earthquake Research Institute, The University of Tokyo), Chairperson:Shiqing Xu(NIED)

3:45 PM - 4:00 PM

[SSS08-14] Supershear rupture induced by step over geometry

*Feng Hu1, Hengxin Ren2, Xiaofei Chen1,2 (1.Univ. of Sci. &Tech. of China, 2.Srn. Univ. of Sci. & Tech.)

Keywords:supershear ruptures can be induced by a fault step over, stress waves radiated from the end of the primary fault control supershear transition on secondary fault segments, rapid rupture speed transitions at step overs in a half-sapce

Based on dynamic rupture simulations on strike-slip step overs in a 3-D full space where the initial shear stresses preclude a supershear transition according to the Burridge-Andrews supershear transition mechanism, we show that rupture speeds can transit from subshear on the primary fault to supershear on the secondary fault for both compressional and extensional step overs. The low normal stress zone and the high shear stress zone, which radiate from the end of the primary fault if its rupture arrest is sudden, coincides beyond the fault step, and determine the supershear rupture occurrence on the secondary fault. However, a low shear stress zone traveling at the shear wave speed is also radiated, making the rupture speed return to subshear in most cases. Sustained supershear rupture are also possible on compressional step overs under certain conditions. Self-arresting ruptures are observed in the overlap area on the secondary fault. In the homogeneous half-space model where supershear rupture exists on the primary fault, because of the free-surface, the rupture speed on the secondary fault rapidly transits to subshear near the fault step if its width exceeds a critical value. The distribution of peak ground velocities are also investigated.