Rupture Directivity of the 25 October 2022 Mw 5.1 Alum Rock Earthquake

E. Hirakawa, G. Parker, A. Baltay, T. Hanks
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引用次数: 1

Abstract

The 25 October 2022 Mw 5.1 Alum Rock earthquake shows strong evidence for southeast rupture directivity along the central Calaveras fault (CCF), as indicated by observed ground motions and simulated kinematic ruptures. Peak ground accelerations (PGAs) and peak ground velocities (PGVs) are notably higher to the southeast, with an order of magnitude difference for stations at the same distance but different azimuths. In addition, PGAs are lower than that predicted by ground-motion models by a factor of 3 on average in all the directions, indicating a low stress drop (∼1.57 MPa). Directivity function modeling and ground-motion simulations both indicate rupture propagation to the southeast with rupture velocity between 2.3 and 2.5 km/s. We suggest that the southward rupture propagation and relatively low stress drop may be typical of M ∼5 earthquakes on this portion of the CCF.
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2022年10月25日5.1 Mw明矾岩地震的破裂方向
根据观测到的地面运动和模拟的运动学破裂,2022年10月25日发生的5.1兆瓦明明岩地震显示了沿卡拉维拉斯断层(CCF)中部的东南断裂指向性的有力证据。东南方向的峰值加速度(PGAs)和峰值速度(PGVs)明显更高,相同距离不同方位角的台站之间存在一个数量级的差异。此外,在所有方向上,PGAs都比地震动模型预测的平均值低3倍,表明应力降较低(约1.57 MPa)。指向性函数模拟和地震动模拟均表明,破裂向东南方向传播,破裂速度在2.3 ~ 2.5 km/s之间。我们认为向南的破裂传播和相对较低的应力降可能是CCF这部分M ~ 5级地震的典型特征。
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