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Inversion of source parameters for moderate and small earthquakes in Beijing region
引用本文:兰从欣,刘杰,郑斯华,马士振,李菊珍. Inversion of source parameters for moderate and small earthquakes in Beijing region[J]. 地震学报(英文版), 2005, 18(5): 532-543. DOI: 10.1007/s11589-005-0032-x
作者姓名:兰从欣  刘杰  郑斯华  马士振  李菊珍
作者单位:Earthquake Administration of Beijing Municipality Beijing 100080,China,Institute of Earthquake Science,China Earthquake Administration Beijing 100036,China,Institute of Earthquake Science,China Earthquake Administration Beijing 100036,China,Earthquake Administration of Beijing Municipality Beijing 100080,China,Earthquake Administration of Beijing Municipality Beijing 100080,China
基金项目:Project of Center for Analysis and Prediction of CEA, Key Project of State Science and Technology in the Tenth Five-year Plan (02-03-04), Joint Seismological Science Foundation of China (604022), and Natural Science Founda-tion of Beijing Municipality (8022009).
摘    要:
Introduction Beijing and the adjacent regions is a significant seismically active area and many geoscien- tists have studied to different extents the non-elastic attenuation and source parameters in the area. GAO et al (1986) and ZHUO et al (1990) studied the coda Q in the Beijing region by the method of dominant frequency and mechanical frequency division with the simulated data. With the con- tinuous construction of digital seismic station network, the digital data are more favorably used…

收稿时间:2004-02-07
修稿时间:2005-04-25

Inversion of source parameters for moderate and small earthquakes in Beijing region
LAN Cong-xin,LIU Jie,ZHENG Si-hua,MA Shi-zhen,LI Ju-zhen. Inversion of source parameters for moderate and small earthquakes in Beijing region[J]. Acta Seismologica Sinica(English Edition), 2005, 18(5): 532-543. DOI: 10.1007/s11589-005-0032-x
Authors:LAN Cong-xin  LIU Jie  ZHENG Si-hua  MA Shi-zhen  LI Ju-zhen
Affiliation:1. Earthquake Administration of Be ijing Municipality, Beijing 100080, China
2. Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China
Abstract:
According to the geological structural features, Beijing and the adjacent areas can be divided into two regions of plain in the east and mountain in the west. Among the stations covered by the telemetered digital seismic station network of Earthquake Administration of Beijing Municipality, the stations in the plain area are all borehole ones and the stations in the western mountainous region are all located on the surface bedrock. In the paper, 511 waveform data recorded by the network from Oct. 2001 to Oct. 2004 are used in the researches for the entire Beijing region, the western mountainous region and the eastern plain area, respectively. The Q values are calculated for each area by Atkinson’s method and compared with the existed data. The reliability of the Q values and the reasons for the difference in the Q values are also discussed. Then, the source parameters and site response are inverted by the Moya’s method, in which two models are used. The first model uses the Q values, earthquakes and stations in the sub-areas and the second model uses the Q values, earthquakes and stations in the entire Beijing region. The results indicate that the source parameters and site responses obtained by two models are basically consistent with each other. It also indicates that the source parameters obtained by these methods are not affected by the size of station network. Foundation item: Project of Center for Analysis and Prediction of CEA, Key Project of State Science and Technology in the Tenth Five-year Plan (02-03-04), Joint Seismological Science Foundation of China (604022), and Natural Science Foundation of Beijing Municipality (8022009).
Keywords:source parameters  site response  quality factor  Q value  seismic station network
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