دورية أكاديمية
Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm
| العنوان: | Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm |
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| المؤلفون: | Leyang Wang, Han Li, Ming Pang |
| المصدر: | Geodesy and Geodynamics, Vol 15, Iss 2, Pp 114-121 (2024) |
| بيانات النشر: | KeAi Communications Co., Ltd., 2024. |
| سنة النشر: | 2024 |
| المجموعة: | LCC:Geodesy LCC:Geophysics. Cosmic physics |
| مصطلحات موضوعية: | Gradient based optimizer (GBO), Lushan earthquake, Non-plane fault model, Slid distribution, Geodesy, QB275-343, Geophysics. Cosmic physics, QC801-809 |
| الوصف: | This paper considers setting different dips for different sub-faults to fit the actual rupture situation based on the fault rupture of the 2013 Lushan MS7.0 earthquake. Meanwhile, combined with the coseismic GNSS data of the Lushan earthquake, the source parameters and sliding distribution of the Lushan earthquake fault are inversed. Firstly, we use the gradient based optimizer (GBO) in nonlinear inversion to obtain the source parameters of this seismic fault. The inversion results indicate that the strike of the fault is 206.52°, the dip is 44.10°, the length is 21.92 km, and the depth is 12.79 km. To refine the sliding distribution of the seismic fault, the seismic fault is divided into 3 × 3 sub-faults. Then, we fix the central sub-fault dip of 44.10°; the dip of other sub-faults is obtained by iteration. After that, the model is further divided into a fault layer model composed of 23 × 19 sub fault slices, and using the Matlab fitting function is used to fit the dip of the 23 × 19 sub faults. Finally, the Lushan seismic fault plane is established as a shovel structure with steep upper and gentle lower, steep south and gentle north. The slip distribution inversion results indicate that the depth of the slip peak is 13 km, the corresponding maximum slip momentum is 0.67 m, the seismic moment is 1.10 × 1019 N·m and the corresponding moment magnitude is MW6.66. The results above are consistent with the research results of seismology. |
| نوع الوثيقة: | article |
| وصف الملف: | electronic resource |
| اللغة: | English |
| تدمد: | 1674-9847 |
| Relation: | http://www.sciencedirect.com/science/article/pii/S1674984723000514; https://doaj.org/toc/1674-9847 |
| DOI: | 10.1016/j.geog.2023.05.002 |
| URL الوصول: | https://doaj.org/article/425ade684cc64cb28983b214d426c076 |
| رقم الأكسشن: | edsdoj.425ade684cc64cb28983b214d426c076 |
| قاعدة البيانات: | Directory of Open Access Journals |
Full Text Finder | تدمد: | 16749847 |
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| DOI: | 10.1016/j.geog.2023.05.002 |