Continuous observation data from 24 GPS stations are selected in the area （33.0°N-41.0°N, 95.0°E-105.0°E） for this study （the period is from Jan. 1, 2015 to Jan. 20, 2016）. Three components, NS...Continuous observation data from 24 GPS stations are selected in the area （33.0°N-41.0°N, 95.0°E-105.0°E） for this study （the period is from Jan. 1, 2015 to Jan. 20, 2016）. Three components, NS, EW and UD, of the daily solutions are filtered by the Hilbert-Huang transform （HHT） with frequency band of 5.787×10^-7-7.716 ×10^-8 Hz （20-150 days in period）. And short-term dynamic characteristics of micro displacement before Menyuan M6.4 earthquake are studied by using the temporal dependencies and cross spectrum analysis. The results show that before the earthquake the horizontal undulatory motions are higher than the average level in the series data which indicate the disturbance feature of regional stress before the earthquake. Three GPS stations on Qinghai-Tibet Plateau with their setting perpendicular to the seismogenic fault have consistent movement. The increase of amplitude of the horizontal micro motion observed before the quake is conducive to the earthquake occurrence. However, we could not be sure if the undulatory motion triggered the earthquake. It is quite necessary to build more GPS continuous observation stations and optimize the monitoring network so as to improve the understanding of the shortterm dynamic crustal variation before earthquake.展开更多
为了提高声呐系统对目标方位的分辨能力,本文提出一种分裂阵频域波束形成方法,即超波束互谱测向法。通过将超波束方法得到的方位谱加权到互谱方法得到的波束形成结果上,从而得到最终的波束输出结果。超波束互谱测向方法的优点是既能够...为了提高声呐系统对目标方位的分辨能力,本文提出一种分裂阵频域波束形成方法,即超波束互谱测向法。通过将超波束方法得到的方位谱加权到互谱方法得到的波束形成结果上,从而得到最终的波束输出结果。超波束互谱测向方法的优点是既能够降低主瓣宽度,抑制旁瓣,提高测向分辨力;又能够保留相位信息,为后续谱分析应用提供参考。实验室水池测试结果表明,利用阵元间距为0.016 m的16元均匀直线阵,对于37.5 k Hz的声信号,采用超波束互谱方法进行波束形成与单纯采用互谱方法进行波束形成相比较,在0°和60°方位上的波束主瓣宽度分别减小了3.8°和6.9°,旁瓣幅度降低超过30 d B,测向分辨力得到明显提高,从而验证采用超波束互谱测向方法提高测向分辨力的可行性和有效性。展开更多
基金加拿大地调局(Geological Survey of CanadaClass Grant Agreement+1 种基金K.-Y.Chun)国家自然科学基金(40034010)资助
文摘应用双差定位方法(hypodd)对北美Loma Prieta地区的分属于3个地震丛集的47个地震进行了精确定位.采用交叉谱法精确求取信号的走时差;同时采用人机联做方式在时域调整、修正按自动方式无法准确提取时差的信号,确保每个事件对的走时差精度.重定位后,在几百米的范围内,原来相互重叠的震源位置聚集为三个明显分离的丛集;水平方向的相对位置平均误差为8.5米,震源深度方向的平均误差为23.4 m.
基金funded by the Project of National Natural Science Foundation of China,based on GPS and leveling data simulation and study on the state of seismogenic deformation field and its mechanical characteristics(41274008)the Basic Research Project of Institute the Earthquake Science,China Earthquake Administration,crustal deformation observation experiment and dynamic process simulation research(2014IES010201)
文摘Continuous observation data from 24 GPS stations are selected in the area （33.0°N-41.0°N, 95.0°E-105.0°E） for this study （the period is from Jan. 1, 2015 to Jan. 20, 2016）. Three components, NS, EW and UD, of the daily solutions are filtered by the Hilbert-Huang transform （HHT） with frequency band of 5.787×10^-7-7.716 ×10^-8 Hz （20-150 days in period）. And short-term dynamic characteristics of micro displacement before Menyuan M6.4 earthquake are studied by using the temporal dependencies and cross spectrum analysis. The results show that before the earthquake the horizontal undulatory motions are higher than the average level in the series data which indicate the disturbance feature of regional stress before the earthquake. Three GPS stations on Qinghai-Tibet Plateau with their setting perpendicular to the seismogenic fault have consistent movement. The increase of amplitude of the horizontal micro motion observed before the quake is conducive to the earthquake occurrence. However, we could not be sure if the undulatory motion triggered the earthquake. It is quite necessary to build more GPS continuous observation stations and optimize the monitoring network so as to improve the understanding of the shortterm dynamic crustal variation before earthquake.
文摘为了提高声呐系统对目标方位的分辨能力,本文提出一种分裂阵频域波束形成方法,即超波束互谱测向法。通过将超波束方法得到的方位谱加权到互谱方法得到的波束形成结果上,从而得到最终的波束输出结果。超波束互谱测向方法的优点是既能够降低主瓣宽度,抑制旁瓣,提高测向分辨力;又能够保留相位信息,为后续谱分析应用提供参考。实验室水池测试结果表明,利用阵元间距为0.016 m的16元均匀直线阵,对于37.5 k Hz的声信号,采用超波束互谱方法进行波束形成与单纯采用互谱方法进行波束形成相比较,在0°和60°方位上的波束主瓣宽度分别减小了3.8°和6.9°,旁瓣幅度降低超过30 d B,测向分辨力得到明显提高,从而验证采用超波束互谱测向方法提高测向分辨力的可行性和有效性。
