[1]王伟涛,杨润海,郑定昌,等.云南地区背景噪声互相关函数中体波信号来源初探*[J].地震研究,2011,34(03):0.
WANG Wei-tao,YANG Run-hai,ZHENG Ding-chang,et al.Study on the Origin of the Body Wave Extracted from Ambient Seismic Noise Cross-correlation Function in Yunnan[J].Journal of Seismological Research,2011,34(03):0.
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《地震研究》[ISSN:1000-0666/CN:53-1062/P]
- 卷:
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34
- 期数:
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2011年03期
- 页码:
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0
- 栏目:
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- 出版日期:
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2011-09-28
文章信息/Info
- Title:
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Study on the Origin of the Body Wave Extracted from Ambient Seismic Noise Cross-correlation Function in Yunnan
- 作者:
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王伟涛1; 杨润海2; 郑定昌2; 倪四道3; 王宝善1
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(1.中国地震局地球物理研究所,北京 100081; 2.云南省地震局,云南 昆明 650224;
3.中国科学院测量与地球物理研究所 动力测量重点实验室,湖北 武汉 430077)
- Author(s):
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WANG Wei-tao1; YANG Run-hai2; ZHENG Ding-chang2; NI Si-dao3; WANG Bao-shan1
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(1.Institute of Geophysics, China Earthquake Administration, Beijing 100081, China)(2. Earthquake Administration of Yunnan Province,Kunming 650224,Yunnan,China)(3.Key Laboratory of Dynamic Geodesy, Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077,Hubei,China)
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- 关键词:
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背景噪声; 体波信号; 噪声源; 季节变化
- Keywords:
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ambient noise; body wave signal; noise source; seasonal variation
- 分类号:
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P315.3
- DOI:
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- 摘要:
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利用云南地区43个宽频带地震台站记录的2008~2010年垂直分量数据,计算了台站对间的互相关函数并得到了5~40 s周期的瑞利面波信号。研究发现在5~10 s周期范围内,瑞利面波信号之前存在很强的前驱信号,该信号能量优势频段为0.1~0.2 Hz,其到时接近噪声互相关函数零点,视速度约为30 km/s。该信号到时随季节存在正负交替变化,进一步的质点分析表明该信号为出射角较小的P波信号。参考已有的研究,认为远场地脉动噪声源中的P波信号穿过地球深部到达云南地区,形成了噪声互相关函数中视速度较高的体波信号,并且相关的噪声源位置在冬季和夏季分别位于北太平洋和南印度洋,具有明显的季节性空间变化。
- Abstract:
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Using vertical component records observed at 43 broad-band seismic stations from 2008 to 2010 in Yunnan, we calculate the noise-cross correlation functions between each station-pair and obtain Raleigh surface wave in the period from 5s to 40s. We find that in the period from 5s to 10s, and before Rayleigh wave, there is a strong precursory wave whose dominant frequency band is between 0.1 Hz and 0.2 Hz and whose arrival time is near the zero of cross correlation functions. Moreover its negative arrival-time in Winter alternates with the positive ones in Summer. Through further analysis of particle-motion, we confirm that this wave is P-wave with smaller reflection angle whose apparent velocity is about 30km/s. Referring to the relevant research results, we conclude that originating from the ambient micro-tremor noise source at a teleseismic distance, P-wave travels through deep earth to Yunnan and reaches a higher apparent velocity. The ambient noise source, which locates in South Indian Ocean in Summer and North Pacific Ocean in Winter, varies seasonally and spatially.
备注/Memo
- 备注/Memo:
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收稿日期:2011-03-21
基金项目:中国地震局地球物理研究所基本科研专项(DQJB10A01,DQJB10B20,DQJB11C05)和国家自然科学基金(41004019,40874095)联合资助.
更新日期/Last Update:
1900-01-01