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Dynamic models of earthquake rupture along branch faults of the eastern San Gorgonio Pass region in California using complex fault structure

机译:利用复杂故障结构,加利福尼亚州东部San Gorgonio Pass Region Artring断裂地震破裂的动态模型

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Geologic data suggest that the Coachella Valley segment of the southern San Andreas fault (southern California, USA) is past its average recurrence time period. At its northern edge, this right-lateral fault segment branches into the Mission Creek and Banning strands of the San Andreas fault. Depending on how rupture propagates through this region, there is the possibility of a throughgoing rupture that could lead to the channeling of damaging seismic energy into the Los Angeles Basin. The fault structures and potential rupture scenarios on these two strands differ significantly, which highlights the need to determine which strand provides a more likely rupture path and the circumstances that control this rupture path. In this study, we examine the effect of different assumptions about fault geometry and initial stress pattern on the dynamic rupture process to test multiple rupture scenarios and thus investigate the most likely path(s) of a rupture that starts on the Coachella Valley segment. We consider three types of fault geometry based on the Southern California Earthquake Center Community Fault Model, and we create a three-dimensional finite-element mesh for each of them. These three meshes are then incorporated into the finite-element method code FaultMod to compute a physical model for the rupture dynamics. We use a slip-weakening friction law, and consider different assumptions of background stress, such as constant tractions and regional stress regimes with different orientations. Both the constant and regional stress distributions show that rupture from the Coachella Valley segment is more likely to branch to the Mission Creek than to the Banning fault strand. The fault connectivity at this branch system seems to have a significant impact on the likelihood of a throughgoing rupture, with potentially significant impacts for ground motion and seismic hazard both locally and in the greater Los Angeles metropolitan area.
机译:地质数据表明,圣安德烈亚斯故障(南加州,美国)的Coachella Valley段已经过其平均复发时间。在其北边,这个右侧故障部门分支到Mission Creek和San Andreas Fault的股线。根据如何通过该地区传播的破裂,有可能导致破裂,这可能导致将地震能量损坏到洛杉矶盆地的渠道。这两个股线上的故障结构和潜在的破裂情景显着不同,这突出了确定哪些股线提供更可能的破裂路径以及控制该破裂路径的情况。在这项研究中,我们研究了不同假设关于故障几何和初始应力模式对动态破裂过程的不同假设,以测试多种破裂场景,从而调查始于Coachella谷段的破裂的最可能路径。我们考虑了基于南加州地震中心社区故障模型的三种故障几何形状,我们为每个人创建了三维有限元网。然后将这三个网格结合到有限元方法代码FaultMod中以计算破裂动力学的物理模型。我们使用防滑弱化摩擦法,并考虑背景应力的不同假设,例如具有不同取向的持续诉讼和区域压力制度。恒定和区域的应力分布都表明,山谷山谷段的破裂更有可能分支到使命小溪而不是禁止禁止股线。该分支系统的故障连通性似乎对经过灾害的可能性产生了重大影响,对地面运动和地震危害的可能性显着影响以及在大型洛杉矶大都市地区。

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