Poststack stochastic seismic inversion method based on gaussian-markov prior constraints

CN116702577BActive Publication Date: 2026-08-28CHINA PETROLEUM & CHEMICAL CORP +1
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Patent Information

Application Number
CN202210182891.1
Authority / Receiving Office
CN · China
Patent Type
Patents(China)
Current Assignee / Owner
Filing Date
2022-02-25
Publication Date
2026-08-28
Estimated Expiration
2042-02-25

AI Technical Summary

Technical Problem

[0005]上述叠后随机反演算法大都借助两点地质统计学描述参数之间的空间相关性,然而两点地质统计学需要精确求取变差函数,这是地质统计学反演的难点和重点;另外,两点地质统计学在估计参数的条件均值和条件方差时,需要求解高维克里金方程组,因此当多次迭代模拟时,会严重拖累计算效率

Benefits of technology

[0056]其有益效果在于:利用扩展Metropolise-Hastings算法提高波阻抗反演结果的垂向分辨率,在此基础上,进一步引入高斯-马尔科夫场描述三维波阻抗的空间相关性,提高反演结果的横向连续性。通过利用高斯-马尔科夫场代替两点地质统计学,可有效结合高斯分布的乘积性质,直接给出条件均值和条件方差的显示表达式,整个反演过程可摆脱对地质统计学的依赖,无需求取变差函数以及求解大型克里金方程组,从而进一步提高随机地震反演算法的灵活易用性和计算效率。

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Abstract

The application discloses a poststack stochastic seismic inversion method based on Gaussian-Markov prior constraint. The method can comprise the following steps: setting an inversion parameter, inputting a wavelet, and establishing a low-frequency model for inversion; determining a to-be-inverted trace in a three-dimensional work area; calculating a conditional mean and a conditional variance according to a kth sampling point in the to-be-inverted trace and a Gaussian-Markov prior distribution; constructing a candidate wave impedance vector of the to-be-inverted trace according to a Gaussian distribution determined by the conditional mean and the conditional variance; performing probability transition on the candidate wave impedance vector of the to-be-inverted trace to realize the update of the wave impedance; and updating the wave impedance of all sampling points of all traces in the three-dimensional work area. The application improves the vertical resolution of the wave impedance inversion result by extending the Metropolise-Hastings algorithm, further introduces a Gaussian-Markov field to describe the spatial correlation of the three-dimensional wave impedance, and improves the lateral continuity of the inversion result.
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Citation Information

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