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CAP方法反演震源机制的台站布局等影响探究--以福建仙游M≥3.0级地震事件为例

Research on Influence of Station Layout and Other Factors in Inversion of Focal Mechanism by CAP Method-Taking Fujian Xianyou M≥3.0 Earthquake Event for Example
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摘要 福建地震台网在日常工作中需要用CAP方法快速并产出可靠的震源机制解。然而,CAP方法受台站布局、台站拾取数量等因素的影响,结果也存在着差异性。本文探索台站布局等因素,为快速产出较为可靠的震源机制解提供参考,缩短震源机制解产出用时。结果显示:在信噪比较高和初至震相清晰的波形数据下,福建仙游地震序列可采取震中距50~130km或者震中距50~100km和150~200km相结合反演,效果较佳,与采用TDMT法反演福建仙游ML>3.5级6次地震的结果相似。 The Fujian Seismic Network quickly produces reliable focal mechanism solutions in daily work by using CAP method.However,the CAP method is affected by factors such as the station layout and the picking number of stations,and the results are also different.This article explores factors such as the station layout to provide a reference for the rapid production of more reliable focal mechanism solutions,and to shorten the time required for the production of focal mechanism solutions.The results show that:under the waveform data with high signal-to-noise ratio and clear onset seismic phases,the Xianyou earthquake sequence in Fujian can be inverted with a combination of epicenter distance of 50-130 km or epicenter distance of 50-100 km and 150-200 km,with better effect,which is similar to the inversion results of 6 earthquakes with ML>3.5 magnitude in Xianyou City of Fujian Province by using TDMT method.
作者 张丽娜 Zhang Li-na(Fujian Earthquake Agency,Fuzhou 350003,Fujian Province,China)
机构地区 福建省地震局
出处 《科学与信息化》 2021年第31期186-189,共4页 Technology and Information
关键词 CAP方法 福建仙游 震源机制解 CAP method Xianyou,Fujian focal mechanism solution
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  • 1ZHENG Yong1,2,MA HongSheng3,Lü Jian4,NI SiDao5,LI YingChun6 & WEI ShengJi2 1 Institute of Geodesy and Geophysics,Chinese Academy of Sciences,Wuhan 430077,China,2 Institute of Geophysics,Chinese Earthquake Administration,Beijing 100086,China,3 Institute of Earthquake Science,Chinese Earthquake Administration,Beijing 100086,China,4 Earthquake Administration of Jiangxi Province,Nanchang 330039,China,5 School of Earth and Space Science,University of Science and Technology of China,Hefei 230026,China,6 Earthquake Administration of Jiangsu Province,Nanjing 210014,China.Source mechanism of strong aftershocks (M_s≥5.6) of the 2008/05/12 Wenchuan earthquake and the implication for seismotectonics[J].Science China Earth Sciences,2009,52(6):739-753. 被引量:104
  • 2谢富仁,崔效锋,赵建涛,陈群策,李宏.中国大陆及邻区现代构造应力场分区[J].地球物理学报,2004,47(4):654-662. 被引量:243
  • 3章惠芳.中国东南沿海地区泉汕爆破深地震测深资料的再解释[J]中国地震,1988(02).
  • 4邵世勤,张诚,邓齐赞.多层地壳模型近地震波走时表计算方法及程序设计[J]西北地震学报,1987(01).
  • 5章林云.广东省河源、海丰地区的深部地壳结构[J]华南地震,1983(03).
  • 6汪素云,许忠淮,1985,中国东部大陆的地震构造应力场,地震学报,7(1),17-31.
  • 7Dreger D S,2002,Time-Domain Moment Tensor INVerse Code(TDMT_INVC),Release 1.1.
  • 8Dreger D S,Brain Savage,1999,Aftershocks of the 1952 Kern County,California,earthquake sequence,Bull Seism Soc Am,89(4),1094- 1108.
  • 9Dreger D S,Helmberger D V,1993,Determination of source parameters at regional distances with single station or sparse network data,J Geophys Res,98,8107- 8125.
  • 10Herrmann R B,Wang C Y,1985,A comparison of synthetic seismograms,Bull Seism Soc Am,75,41-56.

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