一次反射波与自由表面多次波联合偏移成像:模拟数据分析

刘鑫池, 耿建华. 一次反射波与自由表面多次波联合偏移成像:模拟数据分析[J]. 海洋地质与第四纪地质, 2019, 39(4): 174-182. doi: 10.16562/j.cnki.0256-1492.2018112701
引用本文: 刘鑫池, 耿建华. 一次反射波与自由表面多次波联合偏移成像:模拟数据分析[J]. 海洋地质与第四纪地质, 2019, 39(4): 174-182. doi: 10.16562/j.cnki.0256-1492.2018112701
LIU Xinchi, GENG Jianhua. Simultaneous migration of primary and free surface multiples: modeling data analysis[J]. Marine Geology & Quaternary Geology, 2019, 39(4): 174-182. doi: 10.16562/j.cnki.0256-1492.2018112701
Citation: LIU Xinchi, GENG Jianhua. Simultaneous migration of primary and free surface multiples: modeling data analysis[J]. Marine Geology & Quaternary Geology, 2019, 39(4): 174-182. doi: 10.16562/j.cnki.0256-1492.2018112701

一次反射波与自由表面多次波联合偏移成像:模拟数据分析

  • 基金项目:
    国家自然科学基金项目“南黄海中、古生界复杂地质构造地震成像理论与方法”(41630964),“压制鬼波的理论方法与应用研究”(41174106)
详细信息
    作者简介: 刘鑫池(1994—),男,硕士研究生,主要从事多次波成像与鬼波压制研究
    通讯作者: 耿建华,教授,主要从事油气储层地球物理研究,E-mail: jhgeng@tongji.edu.cn
  • 中图分类号: P315

  • 周立君编辑

Simultaneous migration of primary and free surface multiples: modeling data analysis

More Information
  • 基于逆时偏移互相关成像条件,一次反射波与自由表面多次波联合偏移成像可以提供更宽的地下照明成像,以弥补一次反射波覆盖不足,同时不需要预测分离多次波,但是,在成像过程中也引入了偏移假象。首先对一次反射波与自由表面多次波联合偏移成像条件进行分析,通过对模拟数据成像结果分析,提出利用多次波信息进行成像,需要用震源子波和相位反转的地震记录作为逆时偏移中的源端波场做正向传播,原始地震记录作为检波端波场做反向传播,方可获得具有自由表面多次波成像贡献的结果。数值试验结果表明,尽管一次反射波与自由表面多次波联合逆时偏移可以提供更宽的地下照明成像,但是,随着自由表面多次波能量的增强,偏移假象也随之增强;当自由表面多次波能量减弱时,尽管偏移假象相应减弱,但是自由表面多次波对宽角照明成像贡献也随之减弱。因此,一次反射波与自由表面多次波联合偏移成像需要更深入研究。

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  • 图 1  一次反射波与自由表面多次波联合偏移成像原理示意图

    Figure 1. 

    图 2  多次波相位对联合偏移的影响

    Figure 2. 

    图 3  单层速度模型

    Figure 3. 

    图 4  正演模拟单炮记录

    Figure 4. 

    图 5  单层模型模拟数据偏移成像

    Figure 5. 

    图 6  单层模型模拟数据偏移成像

    Figure 6. 

    图 7  截断Sigsbee 2B速度模型

    Figure 7. 

    图 8  不同海底速度情况下包含自由表面多次波模拟单炮记录

    Figure 8. 

    图 9  Sigsbee 2B截断速度模型一次反射波与多次波联合偏移成像

    Figure 9. 

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出版历程
收稿日期:  2018-11-27
修回日期:  2019-01-23
刊出日期:  2019-08-28

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