InSAR Inversion of the Source Mechanism of the 23 January 2024 Xinjiang Wushi M<sub>w</sub>7.0 Earthquake

The M<sub>w</sub>7.0 earthquake that occurred on 23 January 2024, in Wushi County, Xinjiang, China, was centered on the Maidan fault, located at the rear edge of the Kalpin reverse-thrust system in the southwestern Tianshan Mountains, at a depth of 13 km. This event caused significant su...

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Main Authors: Mingyang Jin, Yongsheng Li, Yujiang Li
Format: Article
Language:English
Published: MDPI AG 2025-07-01
Series:Remote Sensing
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Online Access:https://www.mdpi.com/2072-4292/17/14/2435
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author Mingyang Jin
Yongsheng Li
Yujiang Li
author_facet Mingyang Jin
Yongsheng Li
Yujiang Li
author_sort Mingyang Jin
collection DOAJ
description The M<sub>w</sub>7.0 earthquake that occurred on 23 January 2024, in Wushi County, Xinjiang, China, was centered on the Maidan fault, located at the rear edge of the Kalpin reverse-thrust system in the southwestern Tianshan Mountains, at a depth of 13 km. This event caused significant surface deformation and triggered a series of secondary geologic hazards. In this study, data from two satellites, Sentinel-1A and LuTan-1, were combined to obtain the coseismic deformation field of the earthquake. The two-step inversion method was applied to determine the geometrical parameters and slip characteristics of the mainshock fault. The results indicate that the seismicity is primarily driven by reverse faulting, with a contribution from sinistral strike–slip faulting, and the maximum dip–slip displacement is 4.2 m. Additionally, an aftershock of magnitude 5.7 occurring on January 30 was identified in the LT-1 data. This aftershock was controlled by a reverse fault dipping opposite to the mainshock fault, and its maximum slip is 0.65 m. Analysis of the Coulomb stress triggering effect suggests that the Wushi earthquake may have induced the aftershock.
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spelling doaj-art-007e69e00ecb43d482b4cd28fa7881582025-08-20T03:07:58ZengMDPI AGRemote Sensing2072-42922025-07-011714243510.3390/rs17142435InSAR Inversion of the Source Mechanism of the 23 January 2024 Xinjiang Wushi M<sub>w</sub>7.0 EarthquakeMingyang Jin0Yongsheng Li1Yujiang Li2National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100086, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100086, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100086, ChinaThe M<sub>w</sub>7.0 earthquake that occurred on 23 January 2024, in Wushi County, Xinjiang, China, was centered on the Maidan fault, located at the rear edge of the Kalpin reverse-thrust system in the southwestern Tianshan Mountains, at a depth of 13 km. This event caused significant surface deformation and triggered a series of secondary geologic hazards. In this study, data from two satellites, Sentinel-1A and LuTan-1, were combined to obtain the coseismic deformation field of the earthquake. The two-step inversion method was applied to determine the geometrical parameters and slip characteristics of the mainshock fault. The results indicate that the seismicity is primarily driven by reverse faulting, with a contribution from sinistral strike–slip faulting, and the maximum dip–slip displacement is 4.2 m. Additionally, an aftershock of magnitude 5.7 occurring on January 30 was identified in the LT-1 data. This aftershock was controlled by a reverse fault dipping opposite to the mainshock fault, and its maximum slip is 0.65 m. Analysis of the Coulomb stress triggering effect suggests that the Wushi earthquake may have induced the aftershock.https://www.mdpi.com/2072-4292/17/14/2435InSARWushi earthquakeinversionSentinel-1Lutan-1
spellingShingle Mingyang Jin
Yongsheng Li
Yujiang Li
InSAR Inversion of the Source Mechanism of the 23 January 2024 Xinjiang Wushi M<sub>w</sub>7.0 Earthquake
Remote Sensing
InSAR
Wushi earthquake
inversion
Sentinel-1
Lutan-1
title InSAR Inversion of the Source Mechanism of the 23 January 2024 Xinjiang Wushi M<sub>w</sub>7.0 Earthquake
title_full InSAR Inversion of the Source Mechanism of the 23 January 2024 Xinjiang Wushi M<sub>w</sub>7.0 Earthquake
title_fullStr InSAR Inversion of the Source Mechanism of the 23 January 2024 Xinjiang Wushi M<sub>w</sub>7.0 Earthquake
title_full_unstemmed InSAR Inversion of the Source Mechanism of the 23 January 2024 Xinjiang Wushi M<sub>w</sub>7.0 Earthquake
title_short InSAR Inversion of the Source Mechanism of the 23 January 2024 Xinjiang Wushi M<sub>w</sub>7.0 Earthquake
title_sort insar inversion of the source mechanism of the 23 january 2024 xinjiang wushi m sub w sub 7 0 earthquake
topic InSAR
Wushi earthquake
inversion
Sentinel-1
Lutan-1
url https://www.mdpi.com/2072-4292/17/14/2435
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AT yongshengli insarinversionofthesourcemechanismofthe23january2024xinjiangwushimsubwsub70earthquake
AT yujiangli insarinversionofthesourcemechanismofthe23january2024xinjiangwushimsubwsub70earthquake