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沉积盆地地区地壳结构估计——预测反褶积方法消除接收函数多次波混响
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  • 英文篇名:Estimation of the crustal structure beneath the sedimentary Basin:Predictive deconvolution method to remove multiples reverberations of the receiver function
  • 作者:朱洪翔 ; 田有 ; 刘财 ; 冯晅
  • 英文作者:ZHU HongXiang;TIAN You;LIU Cai;FENG Xuan;College of Geo-exploration Science and Technology,Jilin University;Key Laboratory of Applied Geophysics;National-Local Joint Engineering Laboratory of In-situ Conversion,Drilling and Exploitation Technology for Oil Shale;
  • 关键词:接收函数 ; 沉积盆地 ; 多次波混响 ; 预测反褶积 ; H-κ叠加
  • 英文关键词:Receiver function;;Sedimentary basin;;Reverberations;;Predictive deconvolution;;H-κ stacking
  • 中文刊名:DQWX
  • 英文刊名:Chinese Journal of Geophysics
  • 机构:吉林大学地球探测科学与技术学院;国土资源部应用地球物理重点实验室;油页岩地下原位转化与钻采技术国家地方联合工程实验室;
  • 出版日期:2018-09-11
  • 出版单位:地球物理学报
  • 年:2018
  • 期:v.61
  • 基金:国家重点研发计划(2017YFC0601301);; 国家自然科学基金项目(41474030);; 地质调查项目(DD20160207)联合资助
  • 语种:中文;
  • 页:DQWX201809015
  • 页数:12
  • CN:09
  • ISSN:11-2074/P
  • 分类号:156-167
摘要
接收函数方法被广泛地应用于地壳上地幔结构的研究中,H-κ叠加方法是其中最常用的方法之一.对于布设在基岩区台站计算的接收函数,H-κ叠加方法可以准确地估计台站下方地壳厚度和平均波速比,但是对于沉积盆地地区计算的接收函数,由于低速沉积层内会产生多次波混响,干扰甚至覆盖接收函数中莫霍面的转换波和多次波震相,从而影响H-κ叠加结果的准确性.为准确估计沉积盆地地区地壳结构,本文提出使用预测反褶积方法去除接收函数中低速沉积层内多次波混响,其中预测步长由接收函数归一化自相关函数获得,物理意义为沉积层内S波双程走时.合成接收函数和实测接收函数试验表明,本文提出的预测反褶积方法可以有效地去除沉积层多次波混响,并结合改进的H-κ叠加方法可以准确地估计沉积层下覆地壳厚度和平均波速比.相比于其他去除接收函数多次波混响的方法,本文提出的预测反褶积方法具有参数设定简单、运算量小、震相幅值较大等特点,适用于大批量数据处理.
        Recently,the receiver function technique has been widely applied to investigate the layered structures of the crust and upper mantle,and the H-κ stacking is one of the commonly used methods.H-κ stacking method is effective to estimate the crustal thickness and average VP/VSratio beneath a station lying on the bedrock,however,for the stations on sedimentary basin,the presence of low-velocity sedimentary layer can give rise to strong reverberations in theobserved receiver functions,usually influencing and even masking the useful phases from Moho discontinuity.In order to accurately measure the crustal thickness and VP/VSratio beneath the sedimentary basin,we propose a predictive deconvolution method to remove the near-surface reverberations.Autocorrelation of single receiver function is first applied to determine the prediction step length,which is defined by the two-way S wave travel-time in the sedimentary layer.Synthetic and observed receiver function tests show that the near-surface reverberations can be effectively removed by applying predictive deconvolution method,and the processed receiver functions are suitable to accurately estimate the subsediment crustal thickness and VP/VS ratio using an improved H-κ stacking method.Comparing to previous methods applied to eliminate near-surface reverberations,the proposed method has the characteristics of fewer input parameters,less computational complexity and more obvious phases,which is suitable for mass data processing.
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