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    融合深度域加权叠加的ISPE深度域地震子波提取方法及应用

    Integrated depth-domain weighted stacking method and ISPE for depth-domain seismic wavelet extraction: methodology and application

    • 摘要: 深度域地震子波是地下介质速度场的动态响应函数,其波形具有显著的深变特征。该深变特征使得深度域地震子波不满足传统褶积模型中的“线性深不变”假设,导致传统时间域地震子波提取方法无法应用到深度域中。针对该问题,本文提出一种融合深度域加权叠加法的迭代分离参数估计法(ISPE)的深度域地震子波提取方法。首先,基于深度域加权叠加法,通过分段三次Hermite插值实现子波形态的垂向连续性;其次,结合非稳态褶积理论构建深变地震子波簇及其Circulant矩阵,直接合成深度域地震记录;最后,在ISPE框架下,引入深度域广义子波模型,以皮尔逊相关系数作为波形相似性量化指标,在降低地震子波提取参数维度的同时精准控制迭代终止条件,实现深度域地震子波的精确提取。模型测试与实际资料应用表明,即使在强噪声干扰、复杂构造条件和地震数据与测井数据有限的情况下,该方法仍能提取出可靠的深度域地震子波。

       

      Abstract: The depth-domain seismic wavelet is the dynamic response function of the subsurface velocity field, and its waveform exhibits significant depth-variant characteristic. This characteristic makes the depth-domain seismic wavelet fail to satisfy the linear depth-invariant assumption in the conventional convolution model, resulting in the inability to apply conventional time-domain seismic wavelet extraction methods to the depth domain. To address this problem, this paper proposes a depth-domain seismic wavelet extraction method that integrates the depth-domain weighted stacking method and the iterative separate parameter estimation (ISPE) method. First, based on the depth-domain weighted stacking method, vertical continuity of the wavelet morphology is achieved through piecewise cubic Hermite interpolation. Second, combined with the non-stationary convolution model, depth-variant wavelet clusters and their Circulant matrices are constructed to directly synthesize depth-domain seismic records. Subsequently, within the ISPE framework, the depth-domain generalized seismic wavelet model is introduced, and the Pearson correlation coefficient is used as a quantitative metric for waveform similarity. This reduces the parameter dimension of seismic wavelet extraction while precisely controlling the iteration termination conditions, achieving accurate extraction of depth-domain seismic wavelets. Model tests and practical data applications show that even under conditions of strong noise interference, complex structural conditions, and limited seismic and well-logging data, this method can still extract reliable depth-domain seismic wavelets.

       

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