On September 5,2022,at Beijing time 12:52 p.m.,an M_(S)6.8 earthquake struck Luding County,GarzêTibetan Autonomous Prefecture,Sichuan Province.The epicenter of the earthquake was at the intersection of the Sichua...On September 5,2022,at Beijing time 12:52 p.m.,an M_(S)6.8 earthquake struck Luding County,GarzêTibetan Autonomous Prefecture,Sichuan Province.The epicenter of the earthquake was at the intersection of the Sichuan-Yunnan,Bayankala,and South China blocks.The tectonic background is extremely complex,and strong earthquakes occur frequently.Based on a predetermined focal location and focal mechanism solution for the earthquake,we reversed the focal depth and rupture process of the earthquake by fitting the teleseismic P and SH waves recorded by the global seismic network.The results show that the focal depth is 16 km,with the main rupture having a length of about 45 km near the epicenter,with a maximum displacement of 1.02 m.Although the rupture mainly propagates from the north–northwest(NNW)to the south–southeast(SSE)along the fault strike,there is a small-scale rupture slip zone at shallow depths in the north–northeast(NNE)direction along the epicenter of the seismogenic fault.This rupture image corresponds to the cluster distribution of aftershocks in the NNW and SSE directions starting from the epicenter,corresponding to the distribution of recorded landslides.The earthquake occurred on the Moxi fault,located in the southeastern section of the Xianshuihe fault.The major tectonic feature in this area is the southeastward movement of the Chuandian block relative to the Bayanhar block.展开更多
Xinqiao Gully is located in the area of the 2008 Wenchuan M_(s)8.0 earthquake in Sichuan province,China.Based on the investigation of the 2023"6-26"Xinqiao Gully debris flow event,this study assessed the eff...Xinqiao Gully is located in the area of the 2008 Wenchuan M_(s)8.0 earthquake in Sichuan province,China.Based on the investigation of the 2023"6-26"Xinqiao Gully debris flow event,this study assessed the effectiveness of the debris flow control project and evaluated the debris flow hazards.Through field investigation and numerical simulation methods,the indicators of flow intensity reduction rate and storage capacity fullness were proposed to quantify the effectiveness of the engineering measures in the debris flow event.The simulation results show that the debris flow control project reduced the flow intensity by41.05%to 64.61%.The storage capacity of the dam decreases gradually from upstream to the mouth of the gully,thus effectively intercepting and controlling the debris flow.By evaluating the debris flow of different recurrence intervals,further measures are recommended for managing debris flow events.展开更多
1研究背景将卫星遥感红外资料应用于地震监测,起始于20世纪80年代前苏联科学家。后续国内外学者陆续开展了这方面的研究,提出了涡度、RST、ZS、距平和功率谱等异常提取方法,取得了大量震例和机理方面的研究成果(张元生等,2002;Tramutoli...1研究背景将卫星遥感红外资料应用于地震监测,起始于20世纪80年代前苏联科学家。后续国内外学者陆续开展了这方面的研究,提出了涡度、RST、ZS、距平和功率谱等异常提取方法,取得了大量震例和机理方面的研究成果(张元生等,2002;Tramutoli et al,2005;Ouzounov et al,2007;Freund,2011;Jing et al,2022)。张铁宝等(2016)研究表明,川滇块体东边界带强震前,川滇块体存在显著的超阈值辐射增强异常。利用该地区通过震例总结得到的红外辐射异常特征,持续对川滇块体红外辐射进行了多年跟踪,在2022年9月5日四川泸定M_(S)6.8地震前,川滇块体又再次出现了类似的异常变化。泸定地震发生在川滇块体东边界的鲜水河断裂带磨西段。本研究主要分析泸定地震前红外辐射的异常变化。展开更多
基金the Central Publicinterest Scientific Institution Basal Research Fund(2021IEF0501 and CEAIEF20220205)the National Natural Science Foundation of China(42074100).
文摘On September 5,2022,at Beijing time 12:52 p.m.,an M_(S)6.8 earthquake struck Luding County,GarzêTibetan Autonomous Prefecture,Sichuan Province.The epicenter of the earthquake was at the intersection of the Sichuan-Yunnan,Bayankala,and South China blocks.The tectonic background is extremely complex,and strong earthquakes occur frequently.Based on a predetermined focal location and focal mechanism solution for the earthquake,we reversed the focal depth and rupture process of the earthquake by fitting the teleseismic P and SH waves recorded by the global seismic network.The results show that the focal depth is 16 km,with the main rupture having a length of about 45 km near the epicenter,with a maximum displacement of 1.02 m.Although the rupture mainly propagates from the north–northwest(NNW)to the south–southeast(SSE)along the fault strike,there is a small-scale rupture slip zone at shallow depths in the north–northeast(NNE)direction along the epicenter of the seismogenic fault.This rupture image corresponds to the cluster distribution of aftershocks in the NNW and SSE directions starting from the epicenter,corresponding to the distribution of recorded landslides.The earthquake occurred on the Moxi fault,located in the southeastern section of the Xianshuihe fault.The major tectonic feature in this area is the southeastward movement of the Chuandian block relative to the Bayanhar block.
基金supported by the project of the China Geological Survey(No.DD20221746)the National Natural Science Foundation of China(Grant Nos.41101086)。
文摘Xinqiao Gully is located in the area of the 2008 Wenchuan M_(s)8.0 earthquake in Sichuan province,China.Based on the investigation of the 2023"6-26"Xinqiao Gully debris flow event,this study assessed the effectiveness of the debris flow control project and evaluated the debris flow hazards.Through field investigation and numerical simulation methods,the indicators of flow intensity reduction rate and storage capacity fullness were proposed to quantify the effectiveness of the engineering measures in the debris flow event.The simulation results show that the debris flow control project reduced the flow intensity by41.05%to 64.61%.The storage capacity of the dam decreases gradually from upstream to the mouth of the gully,thus effectively intercepting and controlling the debris flow.By evaluating the debris flow of different recurrence intervals,further measures are recommended for managing debris flow events.
文摘1研究背景将卫星遥感红外资料应用于地震监测,起始于20世纪80年代前苏联科学家。后续国内外学者陆续开展了这方面的研究,提出了涡度、RST、ZS、距平和功率谱等异常提取方法,取得了大量震例和机理方面的研究成果(张元生等,2002;Tramutoli et al,2005;Ouzounov et al,2007;Freund,2011;Jing et al,2022)。张铁宝等(2016)研究表明,川滇块体东边界带强震前,川滇块体存在显著的超阈值辐射增强异常。利用该地区通过震例总结得到的红外辐射异常特征,持续对川滇块体红外辐射进行了多年跟踪,在2022年9月5日四川泸定M_(S)6.8地震前,川滇块体又再次出现了类似的异常变化。泸定地震发生在川滇块体东边界的鲜水河断裂带磨西段。本研究主要分析泸定地震前红外辐射的异常变化。
