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张家口地震台和兴隆地震台地脉动信号初步分析

Preliminary analysis to the signals of ground microtremor in Zhangjiakou and Xinglong Seismostation

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【作者】 张从珍高景春刁桂苓赵英萍宋梦真

【Author】 ZHANG Cong-zhen~1, GAO Jing-chun~1, DIAO Gui-ling~1, ZHAO Ying-ping~1, SONG Meng-zhen~2 (1.Seismological Bureau of Hebei Province, Shijiazhuang 050021, China; 2.Huangbizhuang Seismostation, HSB, Huailu 050224, China)

【机构】 河北省地震局河北省黄壁庄地震台 河北石家庄 050021河北石家庄 050021河北获鹿 050224

【摘要】 选取河北省张家口和兴隆2个台站的数字化地震仪连续1年,每日02~03时的地脉动记录,计算功率谱和自相关函数。结果发现兴隆台脉动谱中有4个比较突出的峰值,分别为0.3Hz、3Hz、8Hz、15Hz,张家口台只有3个峰值0.3Hz、3Hz、15Hz。兴隆台UD向的自相关函数呈现出一种比较典型的"红噪声"形态,EW向则呈现出负相关特征,认为可能是只作用于水平向的倾斜脉动的影响。小幅度的仪器干扰信号无论从脉冲标定还是地震波形中都很难发现的,而对脉动进行谱分析则很容易分辨。兴隆台和张家口台地脉动卓越周期时间曲线,基本集中在0.3秒,比较稳定。

【Abstract】 The power spectra and autocorrelation function of the ground microtremor records in Zhangjiakou and Xinglong Seismostation are calculated. The results show that there are 4 peak values in the microtremor spectra of Xinglong Seismostation (0.3Hz, 3Hz, 8Hz,15Hz) and 3 peak values in Zhangjiakou Seismostation (0.3Hz, 3Hz, and 15Hz). The autocorrelation function in the UD direction of Xinglong station showed a typical "red noise" shape, but its EW direction showed negative correlation, which may be the affection of slantwise pulsation that acts on only in horizontal direction. Small instrumental interference signal is hard to distinguish, whether is from pulse calibration or seismic waves, but it is easy in spectral analysis of ground microtremor. The predominant cycle of ground microtremor in the two stations, which concentrated basically in 0.3s, was relatively stable.

【基金】 国家"十五"科技攻关项目(2001BA601B01 01 05);河北省地震局青年科学基金(2003年)
  • 【文献出处】 华北地震科学 ,North China Earthquake Sciences , 编辑部邮箱 ,2004年03期
  • 【分类号】P315.63
  • 【被引频次】3
  • 【下载频次】58
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