地震地质 ›› 1995, Vol. 17 ›› Issue (1): 63-68.

• 科研简报 • 上一篇    下一篇

三峡地区极浅源地震振动波的近场地表效应

马文涛, 胡敏良, 陈献程, 杨清源, 胡平, 赵蒙   

  1. 国家地震局地质研究所, 北京, 100029
  • 收稿日期:1993-10-31 修回日期:1994-05-31 出版日期:1995-03-08 发布日期:2009-11-25
  • 基金资助:
    国家“七·五”攻关项目“长江三峡工程水库诱发地震的研究”专题(16-2-3)的部分成果

SURFACE EFFECTS OF WAVES NEAR-FIELD OF SHALLOW EARTHQUAKES IN THE SANXIA AREA

Ma Wentao, Hu Yuliang, Chen Xiancheng, Yang Qingyuan, Hu Ping, Zhao Meng   

  1. Institute of Geology, SSB, Beijing 100029
  • Received:1993-10-31 Revised:1994-05-31 Online:1995-03-08 Published:2009-11-25

摘要: 通过对三峡地区小台网地震观测和资料研究,认识到该区弹性波地动位移振幅随震中距增加而衰减的变化偏大,地震数字记录的S波波谱分析表明其拐角频率高达21.9Hz,功率谱极大区在0.5~26Hz间,该地区的地震烈度、震中烈度和等震线长轴长度分布具有一定的离散性。上述现象属于极浅源地震波的近场地表效应。研究这些效应特点,可为国家经济建设提供防震、抗震依据。

关键词: 地震观测, 震中烈度, 地震波衰减, 浅源地震, 三峡地区

Abstract: From the near-field observation of microearthquakes and available data,it can be found that the amplitude of displacement decreases with the epicentral distances. The analysis of S-wave spectrum in the digital records indicates that the Goner frequenty is as high as up to 21.9 Hz, with its maximal power spectrum ranging form 0.5-26 Hz, and that the distribution of seismic intensity,epcentral intensity and the longth of major axis of isoseismic line shows certain dispersion,which results from the effect of the near-field surface. Study of these characteristic effect in question can provide a base of earthquake-proof/resisting engineering for economic construction.

Key words: seismological observation, Eqicentral intensity, seismic wave attenuation, Shallow earthquake, Sanxia area