Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation

A Mw 6.6 earthquake struck Menyuan, Qinghai, China, on 7 January 2022. To determine the rupture parameters of this event, the coseismic InSAR deformation fields were mapped and further employed to estimate the focal mechanism. The best-fitting solution emphasized that the 2022 Menyuan earthquake rup...

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Main Authors: Yongsheng Li, Wenliang Jiang, Yujiang Li, Wenhao Shen, Zhongtai He, Bingquan Li, Qiang Li, Qisong Jiao, Yunfeng Tian
Format: Article
Language:English
Published: MDPI AG 2022-04-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/14/9/2111
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author Yongsheng Li
Wenliang Jiang
Yujiang Li
Wenhao Shen
Zhongtai He
Bingquan Li
Qiang Li
Qisong Jiao
Yunfeng Tian
author_facet Yongsheng Li
Wenliang Jiang
Yujiang Li
Wenhao Shen
Zhongtai He
Bingquan Li
Qiang Li
Qisong Jiao
Yunfeng Tian
author_sort Yongsheng Li
collection DOAJ
description A Mw 6.6 earthquake struck Menyuan, Qinghai, China, on 7 January 2022. To determine the rupture parameters of this event, the coseismic InSAR deformation fields were mapped and further employed to estimate the focal mechanism. The best-fitting solution emphasized that the 2022 Menyuan earthquake ruptured at the junction of the Tuolaishan fault and the Lenglongling fault. Both rupturing faults were dominated by sinistral strike-slip, and the main slip was concentrated on the shallow part of the rupture plane. The latter was the main rupture segment with a strike of 106° and a dip of 86°. The slip mainly occurred at depths of 0–8 km, and the rupture was exposed at the surface. The maximum slip reached ~3.5 m, which occurred mainly at a depth of 4 km. Joint analysis of the optimal slip model, relocated aftershocks, Coulomb stress change, and field observation suggested that the strain energy in the Tuolaishan fault may not have been fully released and needs further attention. Moreover, the 2022 Mw6.6 Menyuan earthquake caused a significant stress loading effect on the western Tuolaishan fault and eastern Lenglongling fault, which implies that the 2022 event increased the seismic hazard in these regions.
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spelling doaj.art-97eab6ddd57943459d33b1c1237da2e52023-11-23T09:10:44ZengMDPI AGRemote Sensing2072-42922022-04-01149211110.3390/rs14092111Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field InvestigationYongsheng Li0Wenliang Jiang1Yujiang Li2Wenhao Shen3Zhongtai He4Bingquan Li5Qiang Li6Qisong Jiao7Yunfeng Tian8National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaSchool of Automation, China University of Geoscience, Wuhan 430074, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaNational Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing 100085, ChinaA Mw 6.6 earthquake struck Menyuan, Qinghai, China, on 7 January 2022. To determine the rupture parameters of this event, the coseismic InSAR deformation fields were mapped and further employed to estimate the focal mechanism. The best-fitting solution emphasized that the 2022 Menyuan earthquake ruptured at the junction of the Tuolaishan fault and the Lenglongling fault. Both rupturing faults were dominated by sinistral strike-slip, and the main slip was concentrated on the shallow part of the rupture plane. The latter was the main rupture segment with a strike of 106° and a dip of 86°. The slip mainly occurred at depths of 0–8 km, and the rupture was exposed at the surface. The maximum slip reached ~3.5 m, which occurred mainly at a depth of 4 km. Joint analysis of the optimal slip model, relocated aftershocks, Coulomb stress change, and field observation suggested that the strain energy in the Tuolaishan fault may not have been fully released and needs further attention. Moreover, the 2022 Mw6.6 Menyuan earthquake caused a significant stress loading effect on the western Tuolaishan fault and eastern Lenglongling fault, which implies that the 2022 event increased the seismic hazard in these regions.https://www.mdpi.com/2072-4292/14/9/21112022 Menyuan earthquakeLenglongling faultInSARNE Qinghai-Tibetan Plateauseismic hazard
spellingShingle Yongsheng Li
Wenliang Jiang
Yujiang Li
Wenhao Shen
Zhongtai He
Bingquan Li
Qiang Li
Qisong Jiao
Yunfeng Tian
Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation
Remote Sensing
2022 Menyuan earthquake
Lenglongling fault
InSAR
NE Qinghai-Tibetan Plateau
seismic hazard
title Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation
title_full Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation
title_fullStr Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation
title_full_unstemmed Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation
title_short Coseismic Rupture Model and Tectonic Implications of the January 7 2022, Menyuan Mw 6.6 Earthquake Constraints from InSAR Observations and Field Investigation
title_sort coseismic rupture model and tectonic implications of the january 7 2022 menyuan mw 6 6 earthquake constraints from insar observations and field investigation
topic 2022 Menyuan earthquake
Lenglongling fault
InSAR
NE Qinghai-Tibetan Plateau
seismic hazard
url https://www.mdpi.com/2072-4292/14/9/2111
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