Holocene Activity Characteristics and Seismic Risk of Major Earthquakes in the Middle Segment of the Jinshajiang Fault Zone, East of the Qinghai–Tibetan Plateau
The Jinshajiang fault zone is the western boundary fault of the Sichuan–Yunnan block, located east of the Qinghai–Tibetan Plateau. It is a complex tectonic suture belt with multi-phase activity and is characterized by multiple sets of parallel or intersecting faults. Using high-resolution image inte...
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2024-12-01
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| author | Mingjian Liang Naifei Luo Yunxi Dong Ling Tan Jinrong Su Weiwei Wu |
| author_facet | Mingjian Liang Naifei Luo Yunxi Dong Ling Tan Jinrong Su Weiwei Wu |
| author_sort | Mingjian Liang |
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| description | The Jinshajiang fault zone is the western boundary fault of the Sichuan–Yunnan block, located east of the Qinghai–Tibetan Plateau. It is a complex tectonic suture belt with multi-phase activity and is characterized by multiple sets of parallel or intersecting faults. Using high-resolution image interpretation, seismic geological surveys, and trench studies, we examined the Holocene activity and obtained the paleoseismic sequences on the middle segment of the fault zone. Thus, we could analyze the kinematic characteristics of the fault and its potential risk of strong earthquakes. Our results indicated that the predominant movement of the fault zone was strike-slip motion. In the Jinshajiang fault zone, the Late Quaternary horizontal slip rates of the north-northeast-trending Yarigong fault and the northeast-trending Ciwu fault were 3.6 ± 0.6 mm/a and 2.5 ± 0.5 mm/a, respectively. Three paleoseismic events were identified on the Yarigong fault, dated 6745–3848, 3742–1899, and 1494–1112 cal BP, and on the Ciwu fault, constrained to 32,566–29,430, 24,056–22,990, and 2875–2723 cal BP. The last major earthquake on the Ciwu fault occurred approximately 2800 years ago; therefore, its future seismic hazard deserves attention. |
| format | Article |
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| institution | Kabale University |
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| language | English |
| publishDate | 2024-12-01 |
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| spelling | doaj-art-2a2bf6606d4648f88741eaf59003d9ab2025-01-10T13:14:08ZengMDPI AGApplied Sciences2076-34172024-12-01151910.3390/app15010009Holocene Activity Characteristics and Seismic Risk of Major Earthquakes in the Middle Segment of the Jinshajiang Fault Zone, East of the Qinghai–Tibetan PlateauMingjian Liang0Naifei Luo1Yunxi Dong2Ling Tan3Jinrong Su4Weiwei Wu5Sichuan Earthquake Agency, Chengdu 610041, ChinaThe 9th Geological Brigade of Sichuan Province, Chengdu 618000, ChinaSichuan Earthquake Agency, Chengdu 610041, ChinaSichuan Earthquake Agency, Chengdu 610041, ChinaSichuan Earthquake Agency, Chengdu 610041, ChinaSichuan Earthquake Agency, Chengdu 610041, ChinaThe Jinshajiang fault zone is the western boundary fault of the Sichuan–Yunnan block, located east of the Qinghai–Tibetan Plateau. It is a complex tectonic suture belt with multi-phase activity and is characterized by multiple sets of parallel or intersecting faults. Using high-resolution image interpretation, seismic geological surveys, and trench studies, we examined the Holocene activity and obtained the paleoseismic sequences on the middle segment of the fault zone. Thus, we could analyze the kinematic characteristics of the fault and its potential risk of strong earthquakes. Our results indicated that the predominant movement of the fault zone was strike-slip motion. In the Jinshajiang fault zone, the Late Quaternary horizontal slip rates of the north-northeast-trending Yarigong fault and the northeast-trending Ciwu fault were 3.6 ± 0.6 mm/a and 2.5 ± 0.5 mm/a, respectively. Three paleoseismic events were identified on the Yarigong fault, dated 6745–3848, 3742–1899, and 1494–1112 cal BP, and on the Ciwu fault, constrained to 32,566–29,430, 24,056–22,990, and 2875–2723 cal BP. The last major earthquake on the Ciwu fault occurred approximately 2800 years ago; therefore, its future seismic hazard deserves attention.https://www.mdpi.com/2076-3417/15/1/9Jinshajiang fault zoneHolocene activity characteristicspaleoseismic eventseismic hazardeast of the Qinghai–Tibetan plateau |
| spellingShingle | Mingjian Liang Naifei Luo Yunxi Dong Ling Tan Jinrong Su Weiwei Wu Holocene Activity Characteristics and Seismic Risk of Major Earthquakes in the Middle Segment of the Jinshajiang Fault Zone, East of the Qinghai–Tibetan Plateau Applied Sciences Jinshajiang fault zone Holocene activity characteristics paleoseismic event seismic hazard east of the Qinghai–Tibetan plateau |
| title | Holocene Activity Characteristics and Seismic Risk of Major Earthquakes in the Middle Segment of the Jinshajiang Fault Zone, East of the Qinghai–Tibetan Plateau |
| title_full | Holocene Activity Characteristics and Seismic Risk of Major Earthquakes in the Middle Segment of the Jinshajiang Fault Zone, East of the Qinghai–Tibetan Plateau |
| title_fullStr | Holocene Activity Characteristics and Seismic Risk of Major Earthquakes in the Middle Segment of the Jinshajiang Fault Zone, East of the Qinghai–Tibetan Plateau |
| title_full_unstemmed | Holocene Activity Characteristics and Seismic Risk of Major Earthquakes in the Middle Segment of the Jinshajiang Fault Zone, East of the Qinghai–Tibetan Plateau |
| title_short | Holocene Activity Characteristics and Seismic Risk of Major Earthquakes in the Middle Segment of the Jinshajiang Fault Zone, East of the Qinghai–Tibetan Plateau |
| title_sort | holocene activity characteristics and seismic risk of major earthquakes in the middle segment of the jinshajiang fault zone east of the qinghai tibetan plateau |
| topic | Jinshajiang fault zone Holocene activity characteristics paleoseismic event seismic hazard east of the Qinghai–Tibetan plateau |
| url | https://www.mdpi.com/2076-3417/15/1/9 |
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