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L-Q-T坐标下的P波与S波接收函数联合反演

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文章导航 > 地球学报 > 2022 > 43(5): 719-729

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黄思涵, 董树文, 贺日政, 韩宝福, 周琦, 吴蔚, 牛潇. 2022. L-Q-T坐标下的P波与S波接收函数联合反演[J]. 地球学报, 43(5): 719-729. doi: 10.3975/cagsb.2022.042002
引用本文: 黄思涵, 董树文, 贺日政, 韩宝福, 周琦, 吴蔚, 牛潇. 2022. L-Q-T坐标下的P波与S波接收函数联合反演[J]. 地球学报, 43(5): 719-729. doi: 10.3975/cagsb.2022.042002
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HUANG Si-han, DONG Shu-wen, HE Ri-zheng, HAN Bao-fu, ZHOU Qi, WU Wei, NIU Xiao. 2022. Joint Inversion of P-wave Receiver Functions and S-wave Receiver Functions Based on the L-Q-T Coordinate System. Acta Geoscientica Sinica, 43(5): 719-729. doi: 10.3975/cagsb.2022.042002
Citation: HUANG Si-han, DONG Shu-wen, HE Ri-zheng, HAN Bao-fu, ZHOU Qi, WU Wei, NIU Xiao. 2022. Joint Inversion of P-wave Receiver Functions and S-wave Receiver Functions Based on the L-Q-T Coordinate System. Acta Geoscientica Sinica, 43(5): 719-729. doi: 10.3975/cagsb.2022.042002
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L-Q-T坐标下的P波与S波接收函数联合反演

  • 1. 中国地质科学院, 北京 100037;

  • 2. 北京大学地球与空间科学学院, 北京 100871;

  • 3. 南京大学地球科学与工程学院, 江苏南京 210093

  • 基金项目:

    本文由中国地质调查局地质调查项目(编号: DD20221643-4

    DD20190015)和国家自然科学基金项目(编号: 42074112)联合资助

详细信息
    作者简介: 黄思涵, 男, 1986年生。博士研究生。构造地质学专业。通讯地址: 100037, 北京市西城区百万庄大街26号。E-mail: sihanhuang@hotmail.com
    通讯作者: 董树文, 男, 1954年生。博士, 研究员, 博士生导师。长期从事动力成岩成矿与碰撞造山带研究, 近年来重点探讨燕山运动和东亚大陆地球动力学问题。通讯地址: 100037, 北京市西城区百万庄大街26号。E-mail: swdong@cags.ac.cn

  • 中图分类号: P313.2

Joint Inversion of P-wave Receiver Functions and S-wave Receiver Functions Based on the L-Q-T Coordinate System

  • 1. Chinese Academy of Geological Sciences, Beijing 100037;

  • 2. School of Earth and Space Sciences, Peking University, Beijing 100871;

  • 3. School of Earth Sciences and Engineering, Nanjing University, Nanjing, Jiangsu 210093

More Information
    Corresponding author: DONG Shu-wen

    摘要
  • 接收函数分析是一种研究壳幔结构的主要技术手段。然而, 沉积层引起的多次波会影响壳幔结构特征的可靠研究。与常规Z-R-T坐标下提取接收函数不同, 本文尝试在L-Q-T坐标下提取P波与S波接收函数, 并将二者进行联合反演。通过正演模拟讨论了沉积层厚度对接收函数的影响和实例分析位于具有巨厚沉积的渭河盆地和河套盆地的两个台站, 验证了L-Q-T坐标下提取的P波接收函数能有效显示浅部地壳信息(如沉积层转换波信号), 而 P波与 S波接收函数联合反演能够有效压制沉积层引起的多次波信号。显示了联合反演方法更具优势, 除能获得界面深度信息, 还能获取速度信息。
    Receiver function analysis is a routine method for studying crustal and upper mantle structures.However, sedimentary multiples can negatively impact the accurate determination of crustal and upper mantle structures.In this study, we retrived the receiver functions based on the L-Q-T coordinate system.Then, we conducted joint inversion of P-wave receiver functions (PRFs) and S-wave receiver functions (SRFs) to prove the advantages of this method by providing the case studies of Weihe graben and Hetao graben as well as the illustrative case of the forward modeling results.Our results, on one hand, proved that the L-Q-T coordinate system can present shallow converted crustal signals (e.g., the converted signal of the sedimentary layer), and on the other hand, supported the fact that the simultaneous inversion method was more advantageous for suppressing sedimentary multiples for the more accurate determinantion of the crustal and upper mantle structures.
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收稿日期:  2022-03-04
修回日期:  2022-04-15

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