毛燕, 徐彦, 胡家富, 丛连理, 王彬. 用叠加谱比法研究四川地区Lg尾波Q值的区域性变化[J]. 云南大学学报(自然科学版), 2005, 27(2): 123-128.
引用本文: 毛燕, 徐彦, 胡家富, 丛连理, 王彬. 用叠加谱比法研究四川地区Lg尾波Q值的区域性变化[J]. 云南大学学报(自然科学版), 2005, 27(2): 123-128.
MAO Yan, XU Yan, HU Jia-fu, CONG Lian-li, WANG Bin. Regional variation of Lg coda Q in Sichuan region using stack spectral ratio method[J]. Journal of Yunnan University: Natural Sciences Edition, 2005, 27(2): 123-128.
Citation: MAO Yan, XU Yan, HU Jia-fu, CONG Lian-li, WANG Bin. Regional variation of Lg coda Q in Sichuan region using stack spectral ratio method[J]. Journal of Yunnan University: Natural Sciences Edition, 2005, 27(2): 123-128.

用叠加谱比法研究四川地区Lg尾波Q值的区域性变化

Regional variation of Lg coda Q in Sichuan region using stack spectral ratio method

  • 摘要: 运用单台叠加谱比法,分析了成都台网4个台站的29个地震记录的垂直分量,反演得出与各射线路径相对应的Lg尾波的Q0值.结果表明:Q0值的分布特征与构造活动性密切相关.在构造活动剧烈的龙门山断裂、鲜水河断裂和安宁河断裂,尤其是在这三大断裂的交汇处,Q0值呈现出相当低的值,约在150~210的范围内.在四川盆地的大部分地区,随着构造活动的减弱,Q0值有所抬升,约为240~270.在四川盆地的东部,Q0值可达300.在离开断裂区的四川北部,Q0值在250~300的范围内变化.

     

    Abstract: The vertical components of 29 earthquake records received by 4 stations of Chengdu Network were analyzed with the single station stack spectral ratio method,and inverted the Lg coda Q0 for each path.Results indicate that the distribution characteristics of Q0 correlates with geotectonics closely.In tectonical active regions including Longmenshan fault,Xianshuihe fault,and Anninghe fault,especially in the junction of the three faults,Q0 exhibits very low values varying from 150-210.In most areas of Sichuan Basin,Q0 somewhat increases,with the decreasing of tectonics whose values being from 240-270.In the east part of Sichuan Basin,Q0 can arrive at 300.In the north part of Sichuan away from fault regions,Q0 varies from 250 to 300.

     

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