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2016年新疆阿克陶M_S6.7地震InSAR同震形变与滑动分布特征 被引量:7
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作者 邱江涛 赵强 林鹏 《地震研究》 CSCD 北大核心 2018年第3期415-422,共8页
2016年11月25日新疆阿克陶M_S6.7地震发生在帕米尔构造结的弧顶地区、木吉断陷盆地西端附近,此次地震主震破裂过程复杂,根据地震波反演确定的震源机制解也存在较大差异。利用InSAR技术处理Sentinel-1SAR影像数据获取了此次地震的同震形... 2016年11月25日新疆阿克陶M_S6.7地震发生在帕米尔构造结的弧顶地区、木吉断陷盆地西端附近,此次地震主震破裂过程复杂,根据地震波反演确定的震源机制解也存在较大差异。利用InSAR技术处理Sentinel-1SAR影像数据获取了此次地震的同震形变场,基于弹性半空间位错模型,确定了断层几何参数和滑动分布模型。结果表明,分布式滑动模型能较好地解释观测到的InSAR地表形变场。本次地震包括了至少2次破裂子事件,分别位于中国地震台网测定的震中以东约7 km处(74.11°E,39.25°N)、以东约33 km处(74.49°E,39.16°N)。地震引起的形变场呈上下对称性分布,最大LOS向形变量为20 cm。地震同震位错以右旋走滑为主,主要的滑动量集中在地下深度0~20 km处,最大滑动量为0.84 m。发震断层为木吉断裂,此次地震显示印度板块的北东向推挤作用在增强。 展开更多
关键词 阿克陶地震 INSAR 同震滑动分布 木吉断裂 震源机制
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Characteristics of InSAR Coseismic Deformation and Slip Distribution of the Akto M_S6. 7 Earthquake,Xinjiang
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作者 QIU Jiangtao ZHAO Qiang LIN Peng 《Earthquake Research in China》 CSCD 2019年第3期503-513,共11页
The Akto MS6. 7 earthquake occurred near the western end of the Muji fault basin in the top of the Pamir syntaxis. The main shock of this earthquake is complicated and the focal mechanism solutions based on the seismi... The Akto MS6. 7 earthquake occurred near the western end of the Muji fault basin in the top of the Pamir syntaxis. The main shock of this earthquake is complicated and the focal mechanism solutions based on the seismic wave inversions are different. Based on the Sentinel-1 SAR data,the coseismal deformation field of the earthquake is obtained by In SAR technique. Based on the elastic half-space dislocation model,the geometrical parameters and the slip distribution model are determined by nonlinear and linear inversion algorithms. The results show that the distributed slip model can well explain the coseismic deformation field. The earthquake includes at least two rupture events,which are located at 7 km(74. 11°E,39. 25°N)and 33 km(74. 49°E,39. 16°N)east from the epicenter according to the CENC. The deformation field caused by the earthquake shows a symmetry distribution,with the maximum LOS deformation of 20 cm. The main seismic slip is concentrated in the 0-20 km depth,and the maximum slip is 0. 84 m. The seismic fault is the Muji fault,and this earthquake indicates that the northeastward push of the Indian plate is enhanced. 展开更多
关键词 The akto earthquake INSAR COSEISMIC slip distribution MUJI fault FOCAL mechanism
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Analysis of Gravity Changes before and after the Akto MS6.7 Earthquake in 2016
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作者 Ailixiati Yushan Liu Daiqin +6 位作者 Li Jie Li Rui Abudutayier Yasen Sun Xiaoxu Zhu Zhiguo Li Guirong Chen Li 《Earthquake Research in China》 CSCD 2018年第3期377-387,共11页
This paper analyzes the characteristics of time sequence changes of gravity points near the epicenter,different changes of measuring lines and gravity changes of measuring areas in point-line-area manner respectively ... This paper analyzes the characteristics of time sequence changes of gravity points near the epicenter,different changes of measuring lines and gravity changes of measuring areas in point-line-area manner respectively with the 5-period mobile gravity data through densified observation by the South Xinjiang Observation Network after the 2015-2016 Akto earthquake in Xinjiang. The gravity observation results before the earthquake indicate that the Wuqia-Bulungkol area near the epicenter presented the trend of gravity value increasing since 2015,but the gravity value decreased half a year before the earthquake,and witnessed a high gradient zone of gravity changes during some periods before the earthquake. The gravity observation results after the earthquake show that there is a trend of opposite changes in gravity difference on the northern and southern sides of Bulunkou,and good correspondence exists between the characteristics of gravity field changes near the epicenter before and after the earthquake and the geologic structure distribution in the area. 展开更多
关键词 akto earthquake GRAVITY CHANGES GRAVITY ANOMALIES
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2016年阿克陶M_S6.7地震地表破裂特征和帕米尔现代构造应力场初步分析 被引量:2
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作者 胡伟华 刘培玄 +1 位作者 杨新红 陈建波 《震灾防御技术》 CSCD 北大核心 2017年第4期767-775,共9页
帕米尔高原位于地中海-喜马拉雅地震带上,晚新生代以来随着印度板块向欧亚板块持续不断地挤压汇聚,其构造运动是欧亚大陆最强烈的地区。高原腹地发育一系列近SN向正断层,包括近SN向的塔什库尔干正断层所处的帕米尔中部现代区域的构造应... 帕米尔高原位于地中海-喜马拉雅地震带上,晚新生代以来随着印度板块向欧亚板块持续不断地挤压汇聚,其构造运动是欧亚大陆最强烈的地区。高原腹地发育一系列近SN向正断层,包括近SN向的塔什库尔干正断层所处的帕米尔中部现代区域的构造应力场以EW向水平拉张为主。2016年11月25日发生的阿克陶M_S 6.7级地震的发震构造为塔什库尔干断层分支的NWW向木吉盆地北缘断层,其具有右旋走滑兼正断性质。地震在震中附近产生同震地表形变带,全长约1km,呈近SN-NNE向水平拉伸,发育近EW—NWW向的张裂缝,为地震破裂的产物,张裂缝的最大水平拉伸位移量和最大垂直位移量分别为46cm和16cm。地表破裂带中的NE和NW向张剪裂缝只是连接贯通这些雁列的张裂缝,其水平相对位移量取决于张裂缝的水平拉伸量和张裂缝之间的几何关系。地表形变带表现的拉张性质与帕米尔高原腹地区域现代应力场最大主压应力为垂直向基本一致,可能与深部热物质上涌造成的上地壳拉伸有关。而地表形变带呈近SN向水平拉张,与区域近EW向拉张应力场之间存在显著差异,这可能是木吉盆地北缘右旋走滑正断层阶区局部应力场调整的结果。 展开更多
关键词 阿克陶地震 地表破裂带 拉张应力 塔什库尔干断层 帕米尔
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新疆阿克陶M_S6.7地震引起的新10井水位同震响应研究 被引量:8
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作者 向阳 孙小龙 杨朋涛 《地震学报》 CSCD 北大核心 2017年第6期899-909,共11页
本文根据新10井数字化高频采样水位仪记录到的2016年11月25日新疆阿克陶MS6.7地震所引起的水震波,对比分析了该井水位与地表垂向运动的相关性特征,并对二者与井-含水层系统水文参数的关系进行了深入探讨.分析结果显示:(1)与地震波信号相... 本文根据新10井数字化高频采样水位仪记录到的2016年11月25日新疆阿克陶MS6.7地震所引起的水震波,对比分析了该井水位与地表垂向运动的相关性特征,并对二者与井-含水层系统水文参数的关系进行了深入探讨.分析结果显示:(1)与地震波信号相似,新疆阿克陶MS6.7地震引起的新10井水震波存在两个显著的周期,即6—10s和15—30s;(2)新10井水震波响应幅度与地表垂向运动幅度整体呈正相关,且在高频阶段(频率大于0.08Hz)二者的振幅比随着频率的减小而增大,表明该井水位对周期大于12s的信号放大效能较高;(3)利用水震波与地震波的振幅比估算新10井观测含水层渗透系数的量级为10-2 cm/s,且在地震波作用过程中含水层的水文参数也存在波动.本研究表明,井水位的同震响应机理较为复杂,在分析水位同震响应特征时,高采样率的水位数据是获得可靠结果与认识的基础. 展开更多
关键词 新疆阿克陶MS6.7地震 水震波 地震波 同震响应机理
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2016年新疆阿克陶6.7级地震前重磁变化特征分析 被引量:5
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作者 陈丽 艾力夏提.玉山 +5 位作者 刘代芹 李杰 李桂荣 李瑞 丁新娟 孙小旭 《地震研究》 CSCD 北大核心 2017年第3期392-398,共7页
利用南天山地区3年的流动重力和流动地磁资料,分析阿克陶6.7级地震前区域重力场与地磁场的异常特征。结果表明:(1)阿克陶6.7级地震前重力场年尺度动态变化图像和差分动态演化图像显示乌恰和布伦口地区均出现较显著的流动重力异常变化;(2... 利用南天山地区3年的流动重力和流动地磁资料,分析阿克陶6.7级地震前区域重力场与地磁场的异常特征。结果表明:(1)阿克陶6.7级地震前重力场年尺度动态变化图像和差分动态演化图像显示乌恰和布伦口地区均出现较显著的流动重力异常变化;(2)地震前岩石圈磁场的水平矢量方向和磁偏角均发生较大变化。 展开更多
关键词 阿克陶6.7级地震 重力场 岩石圈磁场
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A Preliminary Analysis of the Seismogenic Structure of the Akto M_S6. 7 Earthquake Sequence on November 25, 2016
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作者 LIANG Shanshan XU Zhiguo +2 位作者 CHEN Hongfeng ZOU Liye LIU Jingguang 《Earthquake Research in China》 CSCD 2019年第3期418-430,共13页
In this study,data from the Xinjiang regional network and IRIS shared global stations are used to relocate the Akto MS6. 7 earthquake sequence on November 25,2016 by using double difference location method. Three eart... In this study,data from the Xinjiang regional network and IRIS shared global stations are used to relocate the Akto MS6. 7 earthquake sequence on November 25,2016 by using double difference location method. Three earthquakes of MS4. 8,MS6. 7 and MS5. 0 are inverted by using the g CAP method,and the focal mechanism solutions are obtained.According to the results of relocating,the location of the main shock is 39. 22°N,73. 98°E,the distribution of the earthquake sequence is about 70 km in length,and the focal depth is mainly within the range of 5-20 km. The plane and depth profiles of the earthquake sequence show that aftershocks extended in SEE direction after the main shock and the dip angle of fault plane is steep. Focal mechanism results show that the three earthquakes are characterized by strike-slip movement. Based on the results of field geological investigation,it is inferred that the seismogenic fault of the Akto earthquake is Muji fault,which is located at the northernmost end of the Kongur extensional system.The possible cause of this earthquake is that the Indian Plate continues to push northward,and during this compression process,the Indian Plate is affected by the clockwise rotation of the Tarim basin,which causes the accumulation of right-lateral action of the Muji fault,resulting in this earthquake. 展开更多
关键词 akto MS6.7 earthquake earthquake location FOCAL mechanism MUJI fault Kongur EXTENSIONAL system
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Gravity variation before the Akto Ms6.7 earthquake, Xinjiang
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作者 Hongtao Hao Lelin Xing +2 位作者 Minzhang Hu Yufei Han Hui Li 《Geodesy and Geodynamics》 2017年第2期136-140,共5页
The relationship between gravity variation and the Akto Ms6.7 earthquake on November 11, 2016, was studied by use of mobile gravity observation data from the China continental structural environmental monitoring netwo... The relationship between gravity variation and the Akto Ms6.7 earthquake on November 11, 2016, was studied by use of mobile gravity observation data from the China continental structural environmental monitoring network. The result revealed that before the Akto earthquake, a high positive gravity variation was observed in the Pamir tectonic knots region (within a maximum magnitude of approximately +80 microgal), which was consistent with the existing knowledge of gravity abnormality and the locations of strong earthquakes. In view of the recent strong seismic activities in the Pamir tectonic knots region, as well as the strong upward crust movement and compressive strain, it is believed that gravity change in the Pamir tectonic knots region reflects the recent strong seismic activities and crust movement. 展开更多
关键词 The continental tectonics environmental monitoring network of China Gravity variation akto earthquake
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高原季节性冻土区砂土液化探讨——以阿克陶MS6.7地震为例
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作者 姚远 陈杰 +3 位作者 李涛 付博 王浩然 李跃华 《第四纪研究》 CAS CSCD 北大核心 2019年第2期381-390,共10页
2016年11月25日新疆阿克陶县木吉乡发生MS6.7地震,发震构造为公格尔山拉张系北端的木吉断裂,断裂总长度超过100 km,以右旋走滑为主兼有一定的拉张分量。文章在对震区进行了初步的地震地质灾害调查,总结砂土液化和地裂缝在高原季节性冻... 2016年11月25日新疆阿克陶县木吉乡发生MS6.7地震,发震构造为公格尔山拉张系北端的木吉断裂,断裂总长度超过100 km,以右旋走滑为主兼有一定的拉张分量。文章在对震区进行了初步的地震地质灾害调查,总结砂土液化和地裂缝在高原季节性冻土地区的分布及发育特点的基础上,发现:1)在研究区Ⅰ维日麻村的砂土液化主要沿原有泉眼或沿地裂缝发育,沿泉眼形成的砂土液化其喷砂锥的覆盖面积达36.1 m2,占总液化面积的60%,研究区Ⅱ布拉克村的砂土液化则主要是沿草甸的根系喷出,在地表形成大面积的最新涌水结冻特征;2)对研究区Ⅱ布拉克村地裂缝的深度进行统计,反演出区域冻土层厚度,结合探槽揭露的地层剖面,推断冻土层发生大面积地裂缝是因为地震引起冻土层下部融土层发生砂土液化导致土层变形失稳,从而使冻土层发生形变产生一系列规律性的地裂缝。 展开更多
关键词 阿克陶地震 砂土液化 地裂缝 冻土
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