Indexed by CSTPCD
Scopus

Petroleum Science Bulletin ›› 2026, Vol. 11 ›› Issue (1): 54-65. doi: 10.3969/j.issn.2096-1693.2026.01.006

Previous Articles     Next Articles

A reflection waveform inversion method based on de-migrated data of characteristic reflection layer

LIU Nengchao1,2(), WANG Shangxu1,2,*(), WU Bo3, YAO Gang1,*()   

  1. 1 State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum, Beijing 102249, China
    2 College of Geophysics, China University of Petroleum, Beijing 102249, China
    3 Sinopec Geophysical Research Institute, Nanjing 211103, China
  • Received:2025-10-27 Revised:2026-01-15 Online:2026-02-15 Published:2026-02-12
  • Contact: WANG Shangxu, YAO Gang E-mail:lnengchao@qq.com;wangsx@cup.edu.cn;yaogang@cup.edu.cn

基于特征层位反偏移数据的反射波形反演方法

刘能超1,2(), 王尚旭1,2,*(), 吴博3, 姚刚1,*()   

  1. 1 中国石油大学(北京) 油气资源与工程全国重点实验室,北京 102249
    2 中国石油大学(北京) 地球物理学院,北京 102249
    3 中石化石油物探技术研究院有限公司,南京 211103
  • 通讯作者: 王尚旭,姚刚 E-mail:lnengchao@qq.com;wangsx@cup.edu.cn;yaogang@cup.edu.cn
  • 作者简介:刘能超(1979年—),博士研究生,从事地震数据处理、全波形反演建模方面的研究,lnengchao@qq.com
  • 基金资助:
    国家自然科学基金“全波形地震成像与弹性参数同步反演理论及核心算法研究”(U23B20159)

Abstract:

Reflection waveform inversion (RWI) exploits reflected-wave information in seismic data to update the deep background velocity model. By alternately inverting for the migration and tomographic components, RWI not only improves the accuracy of deep velocity model updates but also alleviates the cycle-skipping problem to a certain degree. However, RWI generally requires seismic data with a high signal-to-noise ratio (SNR) and has so far achieved its most successful applications in marine environments. In contrast, land seismic data are often degraded by poor receiver coupling, rugged topography, environmental noise, and strong surface-wave interference, making it difficult to acquire continuous and high-SNR reflection waveforms, which severely limits the applicability of RWI to land data. To address these challenges, this study employs Kirchhoff pre-stack time migration to identify characteristic reflection layer and extract their corresponding common-image gathers (CIGs). The extracted events are then reverse migrated to reconstruct reflected-wave data with enhanced SNR. The reconstructed data are subsequently incorporated into RWI and validated using both synthetic and field data examples. The results demonstrate that the proposed method significantly improves the accuracy of deep background velocity model updates. Furthermore, the strong consistency between the migrated images and the corresponding CIGs confirms the reliability and effectiveness of the reconstructed reflection data for RWI applications. Overall, this method offers a new feasible solution for applying RWI to land seismic data.

Key words: full waveform inversion, reflection waveform inversion, Kirchhoff migration and de-migration, characteristic horizon picking, horizon-based reflection data

摘要:

反射波形反演(Reflection waveform inversion,RWI)主要利用地震数据中的反射波信息,对地下深部背景速度模型进行更新。其通过交替迭代更新偏移分量与层析分量,不仅能够更好的对深层速度模型进行更新,还可在一定程度上能够缓解周期跳跃问题。然而,RWI对数据的信噪比要求较高,目前主要在海洋资料中取得了较好的应用效果。相比之下,陆地数据受检波器耦合、起伏地表、环境噪声及面波干扰等因素影响,往往难以获取波形连续且高信噪比的反射波信息,严重制约了RWI 方法在陆地数据中的应用。为解决上述问题,本文基于Kirchhoff叠前时间偏移,拾取特征层及其对应的共成像道集(Common-image gathers,CIGs),并通过反偏移生成高信噪比的反射波数据。随后,将该数据引入RWI,并在合成数据与实际数据中进行了验证。结果表明,该方法能够有效改善深部背景速度模型的更新精度;同时,偏移成像结果和CIGs的对比进一步证明了所构建反射波数据在 RWI 中的适用性与有效性。总体而言,该方法为RWI在陆地数据中的应用提供了一种新的可行性方案。

关键词: 全波形反演, 反射波形反演, Kirchhoff偏移和反偏移, 特征层位拾取, 特征层位反射波数据

CLC Number: