... with different fault surface traces and fault dips were discussed. We also provided explanations for the unbroken northwestern segment of the QF and the seismic intensity anomaly in the Tonghai basin during the 1970 Tonghai event. Finally, we presented several future potential earthquake scenarios occurring...

... Dongchuan County to Fuxian Lake. The southern segment is located on the southern side of Fuxian Lake and is composed of multiple fault branches to the north of the Jianshui Basin. There is only one fault branch near and to the south of the Jianshui Basin, which is called the Jianshui fault (JSF; Figure 1...

... al. (2022) delved into PDP across various fault dip angles, asperity sizes, and corresponding positions. Similarly, Ji et al. (2022) provided PDP insights for the 1970 Tonghai M S 7.8 earthquake across diverse scenario earthquakes. The PDP illustrates the spatial distribution of velocity pulses...

.../09/08 101.529 23.28 SS 5.9 Sun and Liu (2019) 18 Yunnan‐Tengchong 2011/08/09 98.699 25.0 SS 5.2 Gao and Xu (2015) 19 Yunnan‐Tonghai 2018/08/13 102.709 24.19 SS 5.0 Wang et al. (2018) 20 Yunnan‐Tonghai 2018/08/14 102.709 24.19 SS 5.0 Wang et al. (2018...

..., and extends to Dongchuan (Fig.  1a,b ). The middle segment is divided into east and west approximately parallel branches from Dongchuan to Tonghai, Huaning (Fig.  1a ). The southern segment lies from Tonghai, Huaning to the Honghe fault (Fig.  1a ). In the northern section, no earthquakes with magnitude...

... such as a scarp is present along at least part of the lineament. Lineaments based entirely on straight stretches of river A C FIG. 3. (A) Lower fault is part of the major fault indicated in Figure 4 by a solid line immediately south- east of the Tarim Basin. Upper faults are smaller subsidiary faults. Center...

...Guoxing Chen; Dandan Jin; Jiao Zhu; Jian Shi; Xiaojun Li Abstract Based on the parallel computing cluster platform of the ABAQUS software, a large‐scale 2D finite‐element refined nonlinear modeling approach was used to study seismic site effects in the Fuzhou basin, such as peak ground acceleration...

... tip of the Sapanca fault segment significantly increases the transient stress on the adjoining Sakarya segment across the 1- to 2-km-wide Sapanca step-over, allowing rupture propagation across the basin. An evaluation of 30 historical strike-slip earthquakes involving 59 step-over basins supports our...

... thin lines are the provincial boundaries. White dashed lines represent the tectonic boundaries. MCB, Myanmar Central basin; SC block, South China block; SCB, Sichuan basin; SYR, Sichuan–Yunnan rhombic; YZC, Yangtze craton. Main active blocks: I, Tengchong block; II, Baoshan block; III, Simao block; IV...

.... (1935) . Basin-Range faulting in Pleasant Valley, Nevada , J. Geol. 43 , 690 - 707 . Petersen M. D. Seeber L. Sykes L. R...

.... S2, model 3) from a surface‐wave tomography model in the Chuandian region ( Liu et al. , 2019 ), with shallow velocity adopted from the active source record in the nearby Binchuan basin ( Yang, Duan, et al. , 2021b ). The depth of Moho was inferred from receiver function results using a dense array...

... margin of the Taichung basin, along the contact boundary between the western foothills and the western coastal plain. In this work, P ‐wave velocity is shown in Figure  2b ( Chen et al. , 1998 ). The pulse identification method ( Shahi and Baker, 2014 ) contains classification criteria...

... of the seismic rupture and wave propagation, including directivity effects in near‐fault conditions, amplification effects in heavily sedimented basins, as well as topographic and complex site effects ( Smerzini and Pitilakis, 2018 ). Thus, the PBS has the potential for identifying and expanding our...

... the application of the empirical Green’s function method. The original method can be applied to model directivity and basin effects. However, in its standard form, the method is not directly applicable to the modeling of nonlinear soil effects, because it is based on the linear superposition of the empirical...

.... (2016) . The earthquake data were obtained from the China Earthquake Information Network. The trench locations were obtained from Guo, Han, Mao, et al. (2019 , 2020) . CMF, Changma fault; F1, Huangcheng‐Shuangta fault; F2, Southern Wuwei basin fault; F3, Minle‐Damaying fault; F4, Longshoushan fault...

... and then stabilizes. Furthermore, the mean level of the inelastic attenuation factor Q s is 199.5 f 0.98 . Pertaining to site effects, we observe that at the edge of the Sichuan basin, the amplification of sites in the long‐period part is clearly characterized and tends to stabilize with increasing frequency...