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物探与化探  2025, Vol. 49 Issue (4): 855-868    DOI: 10.11720/wtyht.2025.1137
  方法研究信息处理仪器研制 本期目录 | 过刊浏览 | 高级检索 |
地震干涉法分阶多次波逆时偏移
张宏1(), 姜大建1, 刘鑫2,3(), 牛赟博2,3, 李振春2,3, 徐凯1
1.中国石化石油勘探开发研究院 地球物理技术研究所, 北京 100083
2.中国石油大学(华东) 深层油气全国重点实验室, 山东 青岛 266580
3.中国石油大学(华东) 地球科学与技术学院, 山东 青岛 266580
Reverse time migration of order-divided multiples based on seismic interferometry
ZHANG Hong1(), JIANG Da-Jian1, LIU Xin2,3(), NIU Yun-Bo2,3, LI Zhen-Chun2,3, XU Kai1
1. Research Institute of Geophysical Technology, Petroleum Exploration and Production Research Institute,SINOPEC, Beijing 100083, China
2. State Key Laboratory of Deep Oil and Gas, China University of Petroleum(East China), Qingdao 266580, China
3. School of Geosciences, China University of Petroleum(East China), Qingdao 266580, China
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摘要 

地下介质中的盐丘高速体和高陡构造对传统成像方法构成挑战。在常规地震勘探中,多次波通常被视为噪声加以压制或消除。然而,多次波由于其地下传播路径长、反射角小,所以具备更广的成像范围和更丰富的地下构造信息。地震干涉理论能够正确预测多次波,因此基于地震干涉的多次波逆时偏移方法在复杂地下构造成像中具有重要意义。本文分析了地震干涉的基本原理,推导出相应公式并给出算法,提出了基于地震干涉的多次波预测技术。该技术避免了传统多次波处理方法,提高了成像效率,为后续多次波逆时偏移提供了研究基础。针对常规多次波逆时偏移中存在大量串扰噪声的问题,本文创新性地利用地震干涉原理进行了分阶多次波逆时偏移研究,提出了基于地震干涉的分阶多次波逆时偏移方法,有效改善了多次波成像的串扰噪声问题。数值实验表明,相较于一次波逆时偏移,多次波逆时偏移在盐丘下构造成像方面有明显改善,而基于地震干涉理论的分阶多次波逆时偏移则能进一步压制常规多次波逆时偏移中的串扰噪声,对盐下复杂构造进行准确成像,提高了成像分辨率。

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张宏
姜大建
刘鑫
牛赟博
李振春
徐凯
关键词 多次波成像逆时偏移地震干涉多次波预测分阶多次波    
Abstract

High-velocity salt domes and steeply dipping structures in subsurface media pose challenges to conventional imaging methods.In conventional seismic exploration,multiples are usually treated as noise to be suppressed or eliminated.However,due to their long propagation paths and smaller reflection angles within subsurface media,multiples show a wider imaging range and richer information on subsurface structures.Since seismic interferometry enables accurate prediction of multiples,the reverse time migration(RTM) of multiples based on seismic interferometry is crucial for imaging complex subsurface structures.Based on the analysis of the fundamental principles of seismic interferometry,this study derived the corresponding equations and algorithms.Furthermore,this study proposed a multiple prediction technique based on seismic interferometry.By circumventing conventional multiple processing methods,this technique enhances imaging efficiency, providing a research basis for subsequent RTM of multiples.To address the significant crosstalk noise in conventional RTM,this study innovatively utilized seismic interferometry to explore the RTM of order-divided multiples.Finally,this study proposed a RTM method for order-divided multiples based on seismic interferometry,effectively mitigating the problem of crosstalk noise in multiple imaging.Numerical experiments show that compared to the RTM of primary waves,the RTM of multiples exhibited significant improvements in imaging pre-salt structures.The RTM of order-divided multiples based on seismic interferometry could further suppress the crosstalk noise in conventional RTM,enabling accurate imaging of complex pre-salt structures and improving imaging resolution.

Key wordsmultiple imaging    reverse time migration (RTM)    seismic interferometry    multiple prediction    order-divided multiple
收稿日期: 2024-07-24      修回日期: 2025-04-10      出版日期: 2025-08-20
ZTFLH:  P631.4  
基金资助:中国石油化工股份有限公司科技部项目“准噶尔盆地腹部中下组合地震处理解释关键技术研究”(P23101)
通讯作者: 刘鑫(1997-),男,硕士,主要从事地震波传播与成像方面的研究工作。Email:1205536759@qq.com
作者简介: 张宏(1967-),男,教授级高级工程师,主要从事地震资料处理、解释一体化等方面的技术方法研究与应用工作。Email:zhanghong.syky@sinopec.com
引用本文:   
张宏, 姜大建, 刘鑫, 牛赟博, 李振春, 徐凯. 地震干涉法分阶多次波逆时偏移[J]. 物探与化探, 2025, 49(4): 855-868.
ZHANG Hong, JIANG Da-Jian, LIU Xin, NIU Yun-Bo, LI Zhen-Chun, XU Kai. Reverse time migration of order-divided multiples based on seismic interferometry. Geophysical and Geochemical Exploration, 2025, 49(4): 855-868.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2025.1137      或      https://www.wutanyuhuatan.com/CN/Y2025/V49/I4/855
Fig.1  互易定理模型
Fig.2  稳相点示意
Fig.3  基于地震干涉的多次波构建原理
Fig.4  层状模型的测试结果
a—层状速度模型;b—一次波炮记录;c—原始记录;d—预测多次波炮记录
Fig.5  非层状模型的测试结果
a—非层状速度模型;b—一次波炮记录;c—原始记录;d—预测多次波炮记录
Fig.6  Sigsbee2B模型的测试结果
a—Sigsbee2B模型;b—一次波炮记录;c—原始记录;d—预测多次波炮记录
震源波场 检波点波场
一阶多次波 二阶多次波 三阶多次波
一次反射波 成像 假象 假象
一阶多次波 无成像 成像 假象
二阶多次波 无成像 无成像 成像
Table 1  多次波逆时偏移的成像条件
Fig.7  多次波分阶逆时偏移步骤
Fig.8  基于Sigsbee2B模型的多次波逆时偏移结果对比
Fig.9  实际工区偏移结果对比
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