Zheng Jianchang, Zhang Zhengshuai, Li Xiaohan
Department of Mathematics and Statistics, University of Otago, Dunedin 9054, New Zealand.
Shandong Earthquake Agency, China Earthquake Administration, Jinan 250102, China.
Entropy (Basel). 2024 Dec 28;27(1):16. doi: 10.3390/e27010016.
The 2019 Ridgecrest 7.1 earthquake has received significant attention due to its complex fault activity. It is also noticeable for its 6.4 foreshock sequence. There are intricate dynamic relationships between earthquakes in such vigorous sequences. Based on the relocated catalogue, we adopt the nearest neighbour algorithm to analyze its foreshock and aftershock sequences. Detailed links and family structures of the sequence are obtained. The results show that a 5.0 event at 03:16 (UTC) on 6 July is a direct foreshock of the 7.1 mainshock. It is likely related to barriers on the northwest-striking fault. The 6.4 event on 4 July is characterized as a complex conjugate rupture. Notably, a magnitude 4.0 event occurred on the northwest-striking fault before the 6.4 event, establishing it as a direct foreshock. The Ridgecrest sequence is predominantly influenced by northwest fault activity. It first caused small fractures on the northwest-striking fault. Then, it triggered conjugate slips on the southwest-striking fault. Lastly, it led to larger ruptures on the northwest-striking fault.
2019年里奇克莱斯特7.1级地震因其复杂的断层活动而备受关注。其6.4级的前震序列也很引人注目。在如此活跃的序列中,地震之间存在着复杂的动态关系。基于重新定位的目录,我们采用最近邻算法来分析其前震和余震序列。获得了该序列的详细联系和家族结构。结果表明,7月6日世界协调时03:16发生的5.0级地震是7.1级主震的直接前震。它可能与西北走向断层上的障碍物有关。7月4日发生的6.4级地震的特征是复杂的共轭破裂。值得注意的是,在6.4级地震之前,西北走向断层上发生了一次4.0级地震,使其成为直接前震。里奇克莱斯特序列主要受西北断层活动的影响。它首先在西北走向断层上造成小裂缝。然后,它引发了西南走向断层上的共轭滑动。最后,它导致了西北走向断层上更大的破裂。