Co and postseismic fault slip models of the 2022 MW6.7 Menyuan earthquake reveal conjugated faulting tectonics at the central section of the Lenglongling fault

He, Z.; Xu, W.; Li Zhiwei; Xie, L.; Feng, G.; Fang, N.; Liu, X.; Sun, K.; Chen, Z.; Zhu, Z.

Авторы: He Zilong, Xu Wenbin, Li Zhiwei, Xie Lei, Feng Guangcai, Fang Nan, Liu Xiaoge, Sun Kai, Chen Zhidan, Zhu Zhihui
Журнал: Earthquake Science
Том: 37
Номер: 4
Год издания: 2024
Издательство: Seismological Society of China
Местоположение издательства: China
Первая страница: 277
Последняя страница: 303
DOI: 10.1016/j.eqs.2024.04.008
Аннотация: The 2022 MW6.7 Menyuan earthquake ruptured the western end of the Tianzhu seismic gap, providing an opportunity to study the regional seismogenic characteristics and seismic hazards. Here we use interferometric synthetic aperture radar (InSAR) and seismic data to study the mainshock rupture, early afterslip and the second largest aftershock of the 2022 Menyuan earthquake sequences. Our modeling results show that the mainshock ruptured the Lenglongling fault and the Tuolaishan fault with a maximum slip of ∼3 m. Rapid postseismic transient deformation occurred at the center of the Lenglongling fault. Our afterslip modeling reveals that the majority of afterslip occurred in the deeper part of the Lenglongling fault. A high-angle conjugated faulting event is found at the middle section of the Lenglongling fault. We use the stress inversion to investigate the possible triggering mechanism of the conjugated rupture event. The results indicate the maximum principal stress direction is in ∼222°, forming a ∼22° angle between the conjugated fault of second largest aftershock and the mainshock. The calculated normal stress changes indicate the region is within a pull-apart stress field, which favors such a conjugated rupturing event. Our study will help understand the rupture behavior of such kind of conjugated fault in other regions.
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Co and postseismic fault slip models of the 2022 MW6.7 Menyuan earthquake reveal conjugated faulting tectonics at the central section of the Lenglongling faultстатья Исследовательская статья

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