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2010年智利M_s 8.8地震震相特征分析

Features of seismic phases of the M_s8.8 Chile earthquake in 2010

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【作者】 陈翔邓存华余庆坤李雷黄瑶

【Author】 Chen Xiang~(1)),Deng Cunhua~(1)),Yu Qingkun~(2)),Li lei~(1)) and Huang Yao~(1)) 1) Kunming Seismic Station,Yunnan Province 650204,China 2) Infromation Center for the Earthquake Prevention and Disaster Reduction,Earthquake Administration of Yunnan Province,Kunming 650224,China

【机构】 昆明基准地震台云南省防震减灾信息中心

【摘要】 对昆明地震台数字地震仪记录的2010年2月27日智利M_S 8.8地震的震相进行分析,与格尔木、高台、呼和浩特、成都、银川、兰州、西安等7个地震台记录进行对比,提出智利地震的记录特征、分析难点,并将JB表中Pdif波走时曲线的截止距离从150°延伸到177.8°。

【Abstract】 We analyze the waveform of the M_S8.8 Chile earthquake occurred on February 27,2010, which is recorded by the digital seismometers at Kunming Seismic Station,and contrast it with those recorded by other seismic stations in China such as Geermu,Gaotai,Hohhot, Chengdu,Yinchuan,Lanzhou,and Xi an.Thus,after finding the features of the waveform of the Chile earthquake,we put forward some methods for identifying the difficult seismic phases of the earthquakes in Chile.In addition,we suggest that the maximum distance which the Pdif-phase can travel-defined as 150°in the Jeffreys-Bullen Travel Time Table-can be expanded to 177.8°.

  • 【文献出处】 地震地磁观测与研究 ,Seismological and Geomagnetic Observation and Research , 编辑部邮箱 ,2012年Z2期
  • 【分类号】P315
  • 【被引频次】2
  • 【下载频次】14
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