A post-stack wave impedance inversion method based on a Cauchy distribution, comprising: employing a conventional seismic exploration method to collect seismic data, and conducting conventional processing to obtain post-stack seismic data; conducting horizon picking on the post-stack seismic data to obtain horizon data, and checking, correcting, interpolating and smoothing the horizon of a determined target layer; employing a conventional logging method to obtain the time difference curve and density curve of a logged sound wave; according to the post-stack seismic data, horizon data and known well stratification data, calibrating a time difference curve and density curve of the sound wave of a depth domain as a curve of a time domain, simultaneously generating wave impedance curve data in the time domain in a well, and extracting a seismic wavelet; generating an initial wave impedance model; respectively normalizing wavelet data; acquiring a reflection coefficient sequence of a channel via inversion; deducing, via a definition of a relative wave impedance at an n-th sampling point, to obtain a relationship between the wave impedance and the reflection coefficient, and repeating the above process on all seismic channels to obtain wave impedance inversion results for all channels.
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机译:一种基于柯西分布的叠后波阻抗反演方法,包括:采用常规的地震勘探方法采集地震数据,进行常规处理得到叠后地震数据。对叠后地震数据进行地层拾取,以获得地层数据,并对确定的目标层的地层进行检查,校正,插值和平滑处理;采用传统的测井方法得到测井声波的时差曲线和密度曲线。根据叠后地震数据,层位数据和已知井分层数据,将深度域声波的时差曲线和密度曲线校正为时域曲线,同时生成时域波阻抗曲线数据在井中进行域划分,并提取地震子波;生成初始波阻抗模型;分别归一化小波数据;通过反演获取通道的反射系数序列;通过在第 n I>个采样点处的相对波阻抗的定义,得出波阻抗与反射系数之间的关系,并在所有地震通道上重复上述过程以获得波所有通道的阻抗反演结果。
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