Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm

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 Lu...

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Main Authors: Leyang Wang, Han Li, Ming Pang
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2024-03-01
Series:Geodesy and Geodynamics
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674984723000514
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author Leyang Wang
Han Li
Ming Pang
author_facet Leyang Wang
Han Li
Ming Pang
author_sort Leyang Wang
collection DOAJ
description 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.
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spelling doaj.art-425ade684cc64cb28983b214d426c0762024-02-23T04:59:12ZengKeAi Communications Co., Ltd.Geodesy and Geodynamics1674-98472024-03-01152114121Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithmLeyang Wang0Han Li1Ming Pang2Key Laboratory of Mine Environmental Monitoring and Improving Around Poyang Lake of Ministry of Natural Resources, East China University of Technology, Nanchang 330013, China; School of Surveying and Geoinformation Engineering, East China University of Technology, Nanchang 330013, China; Corresponding author. Key Laboratory of Mine Environmental Monitoring and Improving Around Poyang Lake of Ministry of Natural Resources, East China University of Technology, Nanchang 330013, China.Key Laboratory of Mine Environmental Monitoring and Improving Around Poyang Lake of Ministry of Natural Resources, East China University of Technology, Nanchang 330013, ChinaCollege of Resources and Environment, Shandong Agricultural University, Taian 271018, ChinaThis 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.http://www.sciencedirect.com/science/article/pii/S1674984723000514Gradient based optimizer (GBO)Lushan earthquakeNon-plane fault modelSlid distribution
spellingShingle Leyang Wang
Han Li
Ming Pang
Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm
Geodesy and Geodynamics
Gradient based optimizer (GBO)
Lushan earthquake
Non-plane fault model
Slid distribution
title Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm
title_full Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm
title_fullStr Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm
title_full_unstemmed Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm
title_short Slip distribution inversion of seismic sub-fault dip iteration using gradient based optimizer algorithm
title_sort slip distribution inversion of seismic sub fault dip iteration using gradient based optimizer algorithm
topic Gradient based optimizer (GBO)
Lushan earthquake
Non-plane fault model
Slid distribution
url http://www.sciencedirect.com/science/article/pii/S1674984723000514
work_keys_str_mv AT leyangwang slipdistributioninversionofseismicsubfaultdipiterationusinggradientbasedoptimizeralgorithm
AT hanli slipdistributioninversionofseismicsubfaultdipiterationusinggradientbasedoptimizeralgorithm
AT mingpang slipdistributioninversionofseismicsubfaultdipiterationusinggradientbasedoptimizeralgorithm