基于基追踪的时变子波提取与地震反射率反演
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  • 英文篇名:Time-variant wavelet extraction and seismic reflectivity inversion based on basis pursuit
  • 作者:姚振岸 ; 孙成禹 ; 李红星 ; 杨安根
  • 英文作者:YAO Zhen'an;SUN Chengyu;LI Hongxing;YANG An'gen;Fundamental Science on Radioactive Geology andExploration Technology Laboratory,East China University of Technology;School of Geosciences,China University of Pe-troleum (East China);National Pilot Laboratory for Marine Sciencesand Technology (Qingdao);
  • 关键词:基追踪 ; 谱分解 ; 非平稳广义时变地震子波 ; 地震反演
  • 英文关键词:basis pursuit;;spectral decomposition;;non-stationary time-variant generalized seismic wavelet;;seismic inversion
  • 中文刊名:SYDQ
  • 英文刊名:Oil Geophysical Prospecting
  • 机构:东华理工大学放射性地质与勘探技术国防重点学科实验室;中国石油大学(华东)地球科学与技术学院;青岛海洋科学与技术试点国家实验室;
  • 出版日期:2019-02-15
  • 出版单位:石油地球物理勘探
  • 年:2019
  • 期:v.54
  • 基金:国家自然基金项目“深度偏移地震数据特征剖析与深度域直接反演方法研究”(41874153);; “多相孔隙介质全频段波频散与衰减机制及其应用研究”(41764006);; 国家科技重大专项“复杂目标多尺度资料高精度处理关键技术研究”(2016ZX05006-002)联合资助
  • 语种:中文;
  • 页:SYDQ201901016
  • 页数:9
  • CN:01
  • ISSN:13-1095/TE
  • 分类号:10+151-158
摘要
由于噪声和衰减的影响,地震数据不平稳,即地震信号的频谱从浅到深是逐渐变化的。为了研究地震数据的非平稳性质,基于基追踪谱分解方法进行高分辨率时频分解,通过点谱模拟提取广义地震子波,继而构建时变子波核矩阵和时变子波字典,最终实现非平稳基追踪地震反演。实际资料测试表明,基追踪谱分解广义时变子波提取方法能实现高效井震标定,基于时变子波的非平稳基追踪地震反演结果分辨率更高、地质连续性更强、地质细节展示更详细。
        Seismic data are nonstationary because of noise contamination and energy attenuation during wave propagation,which means that the frequency spectrum of seismic signals changes from shallow to deep formations.In order to capture the non-stationary of seismic data,a time-variant wavelet extraction method is proposed using basis pursuit spectral decomposition and generalized seismic wavelet,in which basis pursuit spectral decomposition would supply high resolution time-frequency spectrum for better time-variant wavelet extraction.Based on time-variant wavelets,wavelet kernel matrix and wave dictionary are constructed,and basis pursuit seismic inversion is executed at last.Field data test shows that the proposed scheme achieves better data resolution,more effective wellto-seismic calibration,better geological continuity,and clearer geological details.
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