Double difference location of the Ludian M S6.5 earthquake sequences in Yunnan province in 2014 (in Chinese). Relocation of the Yushu M s7.1 earthquake and its aftershocks in 2010 from HypoDD. Basic Characteristics of Active Structures on the Qinghai-Tibet Plateau (in Chinese). Fault structure and mechanics of the Hayward Fault, California, from double-difference earthquake locations. A double-difference earthquake location algorithm: Method and application to the Northern Hayward Fault, California. Coseismic surface rupture and seismogenic structure of the 2021–05-22 Maduo (Qinghai) Ms7.4 earthquake (in Chinese). Pan J, Bai M, Li C, Liu F, Li H, Liu D, Chevalier M L, We K, Wang P, Lu H, Chen P, Li C. ![]() Seismogenic fault and coseismic surface deformation of the Maduo Ms7.4 earthquake in Qinghai, China: A quick report (in Chinese). Li Z, Li W, Li T, Xu Y, Su P, Guo P, Sun H, Ha G, Chen G, Yuan Z, Li Z, Li X, Yang L, Ma Z, Yao S, Xiong R, Zhang Y, Gai H, Yin X, Xu W, Dong J. Earth Sci-J China Univ Geosci, 40: 1767–1780 GPS-constrained inversion of slip rate on major active faults in the northeastern margin of Tibet Plateau. Grouping occurrences and probability prediction of the strong earthquakes in Chinese mainland (in Chinese). Rupture segmentation and slip partitioning of the mid-eastern part of the Kunlun Fault, north Tibetan Plateau. Li C X, Xu X W, Wen X Z, Zheng R Z, Chen G H, Yang H, An Y F, Gao X. Slip rate gradients along the eastern Kunlun fault. Kirby E, Harkins N, Wang E, Shi X, Fan C, Burbank D. Investigation on diversity of crustal structures beneath the Bayan Har block (in Chinese). High-resolution 3-D shear wave velocity model of the Tibetan Plateau: Implications for crustal deformation and porphyry Cu deposit formation. Huang S, Yao H, Lu Z, Tian X, Zheng Y, Wang R, Luo S, Feng J. ![]() Relocation of the M8.0 Wenchuan earthquake and its aftershock sequence. Focal mechanisms of the 2013 M w6.6 Lushan, China earthquake and high-resolution aftershock relocations. Han L, Zeng X, Jiang C, Ni S, Zhang H, Long F. Relocation of mainshock and aftershock sequence of the M s7.0 Sichuan Jiuzhaigou earthquake. Chin Sci Bull, 58: 3451–3459įang L, Wu J, Su J, Wang M, Jiang C, Fan L, Wang W, Wang C, Tan X. Relocation of mainshock and aftershock sequences of Ms7.0 Sichuan Lushan earthquake. Sci China Ser D-Earth Sci, 46: 356–372įang L H, Wu J P, Wang W L, Lv Z Y, Wang C Z, Yang T, Cai Y. Basic characteristics of active tectonics of China. We speculate that the KMPJ fault is the main seismogenic fault of the M S7.4 Maduo earthquake.ĭeng Q, Zhang P, Ran Y, Yang X, Min W, Chu Q. The sequence overlaps well with surface trace of the KMPJ fault. The location of the aftershock sequence is close to the eastern section of the Kunlun Mountain Pass-Jiangcuo (KMPJ) fault. There is a NW-trending aftershock zone on the north side of the western section, which may be a branch fault triggered by the mainshock. At the eastern end of the aftershock zone, horsetail-like branch faults show the terminal effect of a large strike-slip fault. There is an aftershock gap located to the southeast of the mainshock epicenter with a scale of approximately 20 km. ![]() The focal depth profiles indicate that the seismogenic fault is nearly vertical and dips to southwest or northeast in different sections, indicating a complex geometry. The aftershocks are mainly distributed along NWW direction with an overall strike of 285°. ![]() The results show that the total length of the aftershock zone is approximately 170 km the mainshock epicenter is located in the center of the aftershock zone, indicating a bilateral rupture. In this study, the aftershock sequence within 8 days after the mainshock was relocated by double difference algorithm. The 2021 Qinghai Maduo M S7.4 earthquake was one of the strongest earthquakes that occurred in the Bayan Har block of the Tibetan Plateau during the past 30 years, which spatially filled in the gap of strong earthquake in the eastern section of the northern block boundary.
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