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兰州地震台阵监测能力研究 被引量:3

The study of monitoring ability of Lanzhou seismic array
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摘要 利用兰州地震台阵与兰州地震台数字化近两年的资料,对地震震相特征和震级进行对比分析,结果发现:地震记录震相特征基本相同,台阵有压低干扰背景和突出地震波信号的功能,说明台阵对记录较微弱地震有优势;在震中距小于1 000 km的范围内,兰州台阵的监测能力较明显高于兰州台,而震中距大于1 000 km时,兰州地震台阵与兰州地震台的监测能力相当。 Using the past two years data of Lanzhou seismic array and Lanzhou Seismic Station,we contracted and analyzed seismic phases features and magnitude.The results show that:①the features of seismic phases between Lanzhou seismic array and Lanzhou Seismic Station are almost the same.However,seismic array have the advantage of recording weaker earthquake,since it can efficiently suppress background noise and interference; ②when epicentral distance less than 1 000 km,monitoring ability of Lanzhou seismic array is significantly higher than Lanzhou Seismic Station,while the epicentral distance is greater than 1 000 km,the monitoring abilities of two are roughly equal.
出处 《地震地磁观测与研究》 2013年第5期248-251,共4页 Seismological and Geomagnetic Observation and Research
基金 中国地震局地震预测研究所基本科研业务专项(2012IESLZ09)资助
关键词 兰州地震台阵 监测能力 对比 Lanzhou seismic array monitoring ability comparison
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  • 1黄显良,朱元清.地震台阵及其数据处理方法[J].地震地磁观测与研究,2005,26(1):62-66. 被引量:8
  • 2周民都.青藏高原东北缘深地震测深研究成果回顾[J].西北地震学报,2006,28(2):189-191. 被引量:16
  • 3Langston C A. 1979. Structure under Mount Rainier, Washington, inferred from teleseismic body waves[J]. J Geophys Res, 84(B4): 4749-4762.
  • 4Langston C A, Hammer J K. 2001. The vertical component P-wave receiver function[J]. Bull Seisrn Soc Amer, 91(6) : 1805-1819.
  • 5Li X Q, Nabelek J L. 1999. Deconvolution of teleseismic body waves for enhancing structure beneath a seismometer array[J]. Bull Seism Soc Amer, 89(1) : 190-201.
  • 6Owens T J, Zandat G, Taylor S R. 1984. Seismic evidence for an ancient rift beneath the Cumberland Plateau, Tennes- see: A detailed analysis of broadband teleseismic P waveforms[J]. J Geophys Res, 89(B9) : 7783-7795.
  • 7Shen X, Ritter J R. 2010. Small scale heterogeneities below the Lanzhou CTBTO seismic array, from seismic wavefield fluctuations[J]. Journal of Seismology, 14(3): 481-493.
  • 8Sheng J, Schuster G T, Pankow K L, Pechmann J C, Nowack R L. 2003. Coherence weighted wavepath migration of teleseismic data[J]. EOS Trans AGU, 84: S11E-0344.
  • 9Tseng T L, Chen W P. 2006. Probing the southern Indian shield with P-wave receiver function profiles[J]. Bull Seism Soc Amer, 96(1): 328-333.
  • 10Wu Q J, Li Y H, Zhang R Q, Zeng R S. 2007. Receiver functions from autoregressive deconvolution[J]. Pure Appl Geophys, 164(11) :2175-2192.

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