Yinghui Yang, Lin Li, Jyr‐Ching Hu, H. Tung, Qian Xu, Xiaoyun Li, Xuanmei Fan, Zhibo Yao, Qian Xu, Qiang Chen, M. Tsai
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引用次数: 0
摘要
2022年9月17-18日,台湾东部纵谷断层东倾蠕动段附近的西倾中央山脉断层发生了6.5级和6.9级双联地震。根据干涉合成孔径雷达和全球定位系统观测得出的断层模型显示,西倾的中央山脉断层断裂是造成这两次主震的原因。同时,这两次大地震导致台湾东部纵谷附近的双聚合板块边界断层发生了~100 公里的断层滑动。2022 年池上地震序列填补了位于 2006 年 ML 6.1 台东地震和 2013 年 ML 6.1 瑞穗地震之间的 CRF 地震缺口。最后,2022 年池上地震序列增加了 CRF 最南段的库仑破坏应力,可能导致未来更高的地震潜力。
Double-Vergent Plate Boundary Faults and Triggered Coseismic Rupture of the 2022 Chihshang Doublet Earthquake Occurred in Eastern Taiwan
The earthquake doublet of Mw 6.5 and 6.9 occurred along the west-dipping Central Range fault (CRF) adjacent to the east-dipping creep segment of the Longitudinal Valley fault in eastern Taiwan on 17–18 September 2022. The faulting model derived from the Interferometric Synthetic Aperture Radar and Global Positioning System observation suggests that the west-dipping CRF rupture is responsible for the two mainshocks. Meanwhile, the two major earthquakes resulted in ∼100 km of fault slip along the double-convergent plate boundary faults near the Longitudinal Valley in eastern Taiwan. The 2022 Chihshang earthquake sequence filled the seismic gap of the CRF located between the 2006 ML 6.1 Taitung earthquake and the 2013 ML 6.1 Ruisui earthquake. Finally, the 2022 Chihshang earthquake sequence increased the Coulomb failure stress in the southernmost segment of the CRF, which may cause a higher seismic potential in the future.