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Ionospheric disturbances associated with the 2015 M7.8 Nepal earthquake 被引量:4
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作者 Yiyan Zhou Jian Yang +3 位作者 Fuying Zhu Fanfan Su Liangchen Hu Wenbo Zhai 《Geodesy and Geodynamics》 2017年第4期221-228,共8页
Based on the total electron content (TEC) derived from Global Positioning System (GPS) observations of the Crustal Movement Observation Network of China (CMONOC) and the Global Ionosphere Map (GIM) from the Ce... Based on the total electron content (TEC) derived from Global Positioning System (GPS) observations of the Crustal Movement Observation Network of China (CMONOC) and the Global Ionosphere Map (GIM) from the Center for Orbit Determination in Europe (CODE), we detected and analyzed the ionospheric variations during the 2015 M7.8 Nepal earthquake (including the pre-earthquake ionospheric anomalies and coseismic ionospheric disturbances (CIDs) following the main shock). The analysis of vertical total electron content (VTEC) time series shows that the large-scale ionospheric anomalies appeared near the epicenter two days prior to the earthquake. Moreover, the pre-earthcluake ionospheric anomalies were also observed in the geomagnetically conjugated region. In view of solar-terrestrial environment, the pre-earthquake ionospheric anomalies could be associated with the Nepal earthquake. In addition, we also detected the CIDs through the high-frequency GPS observation stations. The CIDs had obvious oscillated waveforms with the peak-to-peak disturbance amplitudes of about I TECu and 0.4 TECu, which propagated approximately with the horizontal velocities of 877 ±75 m/s and 319 ± 30 m/s, respectively. The former is triggered directly by the acoustic waves which originated from the energy release of the earthquake near the epicenter, while the latter could be stimulated by the acoustic-gravity waves from the partial transformation of the acoustic waves. 展开更多
关键词 GPS TEC M7.8 nepal earthquake Pre-earthquake ionospheric anomalies CID
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Measuring ground deformations caused by 2015 Mw7.8 Nepal earthquake using high-rate GPS data 被引量:1
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作者 Yong Huang Shaomin Yang +3 位作者 Xuejun Qiao Mu Lin Bin Zhao Kai Tan 《Geodesy and Geodynamics》 2017年第4期285-291,共7页
The April 25, 2015 Mw7.8 Nepal earthquake was successfully recorded by Crustal Movement Observation Network of China (CMONOC) and Nepal Geodetic Array (NGA). We processed the high-rate GPS data (1 Hz and 5 Hz) b... The April 25, 2015 Mw7.8 Nepal earthquake was successfully recorded by Crustal Movement Observation Network of China (CMONOC) and Nepal Geodetic Array (NGA). We processed the high-rate GPS data (1 Hz and 5 Hz) by using relative kinematic positioning and derived dynamic ground motions caused by this large earthquake. The dynamic displacements time series clearly indicated the displacement amplitude of each station was related to the rupture directivity. The stations which located in the di- rection of rupture propagation had larger displacement amplitudes than others. Also dynamic ground displacement exceeding 5 cm was detected by the GPS station that was 2000 km away from the epicenter. Permanent coseismic displacements were resolved from the near-field high-rate GPS stations with wavelet decomposition-reconstruction method and P-wave arrivals were also detected with S transform method. The results of this study can be used for earthquake rupture process and Earthquake Early Warning studies. 展开更多
关键词 High-rate GPS Mw7.8 nepal earthquake Dynamic ground motion Permanent coseismic displacements P-wave arrival detection
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高频GPS测定的尼泊尔M_W7.8和M_W7.3地震震时地表动态变形过程 被引量:2
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作者 黄勇 杨少敏 +4 位作者 乔学军 林牧 赵斌 刘刚 谭凯 《大地测量与地球动力学》 CSCD 北大核心 2017年第3期221-223,229,共4页
以陆态网络和尼泊尔境内高频(1Hz)GPS观测数据为基础,采用动态双差相对定位方法,获取2015年尼泊尔M_W7.8和M_W7.3地震震时近场地表动态变形过程。结果表明,M_W7.8地震震中东侧高频GPS站动态位移幅度明显大于震中西侧;各高频GPS站动态位... 以陆态网络和尼泊尔境内高频(1Hz)GPS观测数据为基础,采用动态双差相对定位方法,获取2015年尼泊尔M_W7.8和M_W7.3地震震时近场地表动态变形过程。结果表明,M_W7.8地震震中东侧高频GPS站动态位移幅度明显大于震中西侧;各高频GPS站动态位移幅度不仅与测站震中距有关,而且与地震破裂传播方向有关;M_W7.3地震引起的水平动态位移相对较小。将高频GPS与邻近强震仪动态位移时序进行对比发现,二者在振幅和相位上具有较好的一致性。 展开更多
关键词 高频GPS 尼泊尔M_W7.8、M_W7.3地震 震时地表动态变形
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2015年4月25日尼泊尔Mw7.8级地震的孕震构造背景和特征 被引量:35
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作者 刘静 纪晨 +4 位作者 张金玉 张培震 曾令森 李占飞 王伟 《科学通报》 EI CAS CSCD 北大核心 2015年第27期2640-2655,共16页
2015年4月25日尼泊尔发生M w7.8级大地震,震源机制解结果一致表明该地震为低角度逆冲型.迄今发生百余次余震,其中包括M s7.0级以上强余震,并触发正断层型小震群.此次地震发生于喜马拉雅碰撞造山带中段,位于1934年比哈-尼泊尔M w^8.1级和... 2015年4月25日尼泊尔发生M w7.8级大地震,震源机制解结果一致表明该地震为低角度逆冲型.迄今发生百余次余震,其中包括M s7.0级以上强余震,并触发正断层型小震群.此次地震发生于喜马拉雅碰撞造山带中段,位于1934年比哈-尼泊尔M w^8.1级和1505年木斯塘M w^8.2级地震之间的地震空区内,是自1950年察隅M w^8.4级地震以来喜马拉雅主逆冲断裂上发生的最大震级地震.为更好地理解这次地震,本文综述喜马拉雅造山带的构造背景、断裂组合构成和几何形态、历史强震分布和破裂范围、现代小地震活动性特征、强震孕育的基本模式、震间加载和同震位移的空间互补性.在简单介绍同震破裂的断面初始解基本特征基础上,初步讨论了这次尼泊尔地震与喜马拉雅带特征型地震的关系,与2008年汶川地震的比较,以及低角度逆冲地震破裂的地表出露和对区域地震危险趋势的指示意义等问题. 展开更多
关键词 喜马拉雅碰撞造山带 喜马拉雅主逆冲断裂 尼泊尔Mw7.8级地震 低角度逆冲型地震 构造背景 强震孕育模式
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