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海拉尔CTBTO地震台阵下方小尺度非均匀体研究
引用本文:沈旭章,张淑珍,郑重,郝春月.海拉尔CTBTO地震台阵下方小尺度非均匀体研究[J].地球物理学报,2010,53(5):1158-1166.
作者姓名:沈旭章  张淑珍  郑重  郝春月
作者单位:1.中国地震局兰州地震研究所, 兰州 730000;2.中国地震局地震预测研究所兰州科技创新基地, 兰州 730000;3.甘肃省地震局兰州观象台, 兰州 730000;4.中国地震局地球物理研究所,北京 100081
基金项目:国家自然基金项目(40904014)和中国地震局地震预测研究所基本科研业务专项(2009A19)资助.
摘    要:利用国际禁核组织在海拉尔布设的小孔径地震台阵的16个深远地震波资料,分离出了P波波场中不相干的尾波.频率域中对波场扰动的研究表明,在0.5~3.0 Hz的频率范围内,观测到的波场扰动可以利用P波在随机介质中的散射进行解释.不同远震事件得到的稳定结果表明,在该台阵下方34 km厚的地壳和110 km厚的岩石层中可能存在相关长度为2.0~7.4 km的散射体.

关 键 词:散射  均匀体  波场扰动  海拉尔CTBTO台阵  
收稿时间:2009-10-09
修稿时间:2010-04-07

Study on the small-scale heterogeneities below the Hailaer CTBTO seismic array
SHEN Xu-Zhang,ZHANG Shu-Zhen,ZHENG Zhong,HAO Chun-Yue.Study on the small-scale heterogeneities below the Hailaer CTBTO seismic array[J].Chinese Journal of Geophysics,2010,53(5):1158-1166.
Authors:SHEN Xu-Zhang  ZHANG Shu-Zhen  ZHENG Zhong  HAO Chun-Yue
Institution:1.Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China;2.Lanzhou Base of Institute of Earthquake Prediction, China Earthquake Administration, Lanzhou 730000, China;3.Lanzhou Observation Station, China Earthquake Administration, Lanzhou 730000, China;4.Institute of Geophysics, China Earthquake Administration, Beijing 100081, China
Abstract:Incoherent seismic wavefield fluctuations recorded by Hailaer CTBTO seismic array are separated from 16 deep teleseismic events. The frequency-dependent intensities of the mean and fluctuation wavefields are analyzed. The observed wavefield fluctuations in the frequency range 0.5~3.0 Hz can be explained by scattering of the teleseismic P-wave front at random media-type structures. The stable and narrow range of the fluctuation parameters from these teleseismic events indicates evidence for scattered seismic phases which are generated inside the crust and lithosphere. The reasonable structural models contain heterogeneities with 2.0~7.4 km correlation lengths in the 34 km thick crust and the 110 km thick lithosphere.
Keywords:Scattering  Heterogeneity  Seismic wavefield fluctuations  Hailaer CTBTO seismic array
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