P波速度对接收函数H-k搜索叠加结果的影响分析

李翠芹, 沈旭章, 秦满忠

李翠芹, 沈旭章, 秦满忠. 2014: P波速度对接收函数H-k搜索叠加结果的影响分析. 地震学报, 36(3): 480-490. DOI: 10.3969/j.issn.0253-3782.2014.03.013
引用本文: 李翠芹, 沈旭章, 秦满忠. 2014: P波速度对接收函数H-k搜索叠加结果的影响分析. 地震学报, 36(3): 480-490. DOI: 10.3969/j.issn.0253-3782.2014.03.013
Li Cuiqin, Shen Xuzhang, Qin Manzhong. 2014: The effect of P wave velocity on the H-k stacking results of receiver functions. Acta Seismologica Sinica, 36(3): 480-490. DOI: 10.3969/j.issn.0253-3782.2014.03.013
Citation: Li Cuiqin, Shen Xuzhang, Qin Manzhong. 2014: The effect of P wave velocity on the H-k stacking results of receiver functions. Acta Seismologica Sinica, 36(3): 480-490. DOI: 10.3969/j.issn.0253-3782.2014.03.013

P波速度对接收函数H-k搜索叠加结果的影响分析

基金项目: 中国地震局地震预测研究所基本科研业务专项(2011IESLZ05)和国家自然科学基金(41274093, 40904014)共同资助.
详细信息
    通讯作者:

    沈旭章, e-mail: shenxzh@gmail.com

  • 中图分类号: P315.3

The effect of P wave velocity on the H-k stacking results of receiver functions

  • 摘要: 从公式推导、 不同模型数值试验和实际资料处理等3个方面, 系统研究了P波速度vPP对接收函数H(地壳厚度)-k(波速比)叠加搜索结果的影响. 结果表明, vPP的变化与H正相关, 与k负相关; 且地壳模型越复杂, vPP对H的影响越大.
    Abstract: This paper systematically investigates the effect of P wave velocity on the H-k stacking results of receiver functions by three aspects of theoretical analyses, numerical tests and observed data processing. The results show that the P wave velocity is positively correlated with crustal depth H, and negatively correlated with wave velocity ratio k. Moreover, the more complex the crust model is, the larger effect P wave velocity has on H.
  • 图  1   单层模型中Ps, PpPs, PpSs+PsPs震相射线路径(左)及接收函数(右)示意图

    Figure  1.   Ray paths of Ps, PpPs and PpSs+PsPs (left panel) and synthetic receiver functions (right panel) for one-layer simple model

    图  2   数值试验的理论地壳模型

    (a) 单层模型; (b) 双层模型; (c) 含梯度带的双层模型

    Figure  2.   Three theoretical crustal models for numerical test

    (a) One-layered model; (b) Two-layered model; (c) Two-layered model with a gradient structure

    图  3   单层模型数值试验结果

    (a) 理论接收函数; (b)、 (c)和(d)分别表示vPP为预设值、 小于预设值0.3 km/s和大于预设值0.3 km/s时H-k方法的搜索结果. 白色“+”为数据计算得到的结果, 黑色圆点表示预设模型; (e)和(f)分别表示数值模拟试验中地壳厚度H和波速比kvPP的变化

    Figure  3.   Numerical test for the one-layer model

    (a) Theoretical receiver functions; (b--d) H-k stacking results with default vPP, smaller vPP (0.3 km/s less than default vPP ) and larger vPP (0.3 km/s larger than default vPP), respectively. The white crosses represent the calculated values, black dots represent the default values, gray bars represent the stacking amplitude of receiver functions;(e) H versus vPP in numerical tests; (f) k versus vPP in numerical tests

    图  4   双层模型数值试验结果

    (a) 理论接收函数; (b)、 (c)和(d)分别表示vPP为预设值、 小于预设值0.3 km/s和大于预设值0.3 km/s时H-k方法的搜索结果.白色“+”为数据计算得到的结果, 黑色圆点表示预设模型; (e)和(f)分别表示数值模拟试验中地壳厚度H和波速比kvPP的变化

    Figure  4.   Numerical test for the two-layered model

    (a) Theoretical receiver functions; (b--d) H-k stacking results with default vPP, smaller vPP (0.3 km/s less than default vPP ) and larger vPP (0.3 km/s larger than default vPP), respectively. The white crosses represent the calculated values, black dots represent the default values, gray bars represent the stacking amplitude of receiver functions; (e) H versus vPP in numerical tests; (f) k versus vPP in numerical tests

    图  5   存在一低速梯度带的双层模型数值试验结果

    (a) 理论接收函数; (b)、 (c)和(d)分别表示vPP为预设值、 小于预设值0.3 km/s和大于预设值0.3 km/s时 H-k方法的搜索结果. 白色“+”为数据计算得到的结果, 黑色圆点表示预设模型; (e)和(f)分别 表示数值模拟试验中地壳厚度H和波速比kvPP的变化

    Figure  5.   Numerical test for the two-layered model with a gradient structure

    (a) Theoretical receiver functions; (b--d) H-k stacking results with default vPP, smaller vPP (0.3 km/s less than default vPP ) and larger vPP (0.3 km/s larger than default vPP), respectively. The white crosses represent the calculated values, black dots represent the default values, gray bars represent the stacking amplitude of receiver functions; (e) H versus vPP in numerical tests; (f) k versus vPP in numerical tests

    图  6   不同vPP值对应的天水台实际资料处理结果

    (a) 天水台观测接收函数; (b), (c), (d)和(e)分别表示vPP为6.10, 6.20, 6.31, 6.38 km/s时H-k的搜索叠加结果

    Figure  6.   Example of TSS station with different vPP

    (a) Observed receiver functions; (b) H-k stacking results with vPP=6.10 km/s; (c) H-k stacking results with vPP=6.20 km/s; (d) H-k stacking results with vPP=6.31 km/s; (e) H-k stacking results with vPP=6.38 km/s

    图  7   3种模型中vPP及vPP变化率对H-k结果的影响

    (a) HvPP关系; (b) H变化率与vPP变化率关系; (c) k值与vPP关系; (d) k变化率与vPP变化率关系

    Figure  7.   The influence of vPP and variation rate of vPP on the H-k results for the three models

    (a) H versus vPP; (b) The variation rate of H versus the variation rate of vPP; (c) k versus vPP; (d) The variation rate of k versus the variation rate of vPP

    表  1   天水台各模型的接收函数H-k方法搜索结果

    Table  1   H-k stacking results of TSS station for three different models

    下载: 导出CSV
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  • 收稿日期:  2013-05-02
  • 修回日期:  2013-07-15
  • 发布日期:  2014-04-30

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