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Kirchhoff型偏移反偏移串联地震数据炮检距转换技术

本站小编 Free考研考试/2022-01-03

叶云飞1,3,,
孙建国2,,,
刘志斌3,
张益明3,
孙文博3,
仝中飞3
1. 吉林大学南方研究院, 广东珠海 519090
2. 吉林大学地球探测科学与技术学院, 长春 130026
3. 中海油研究总院有限责任公司, 北京 100027

基金项目: 国家自然科学基金项目(41274120)和十三五国家重大专项"南海深水区油气勘探地球物理关键技术课题"(2016ZX05026001)联合资助


详细信息
作者简介: 叶云飞, 男, 1982年生, 高级工程师, 主要从事海洋油气地震勘探工作.E-mail:yeyf2@cnooc.com.cn
通讯作者: 孙建国, 男, 1956年生, 教授, 主要从事波动理论与成像技术、地震资料处理方法与解释技术等方面的教学和研究工作.E-mail:sun_jg@jlu.edu.cn
中图分类号: P631,P738

收稿日期:2018-02-02
修回日期:2018-07-13
上线日期:2018-09-05



Conversion of seismic data offset by series Kirchhoff migration and demigration

YE YunFei1,3,,
SUN JianGuo2,,,
LIU ZhiBin3,
ZHANG YiMing3,
SUN WenBo3,
TONG ZhongFei3
1. South Institute of Jilin University, Guangdong Zhuhai 519090, China
2. College for Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China
3. CNOOC Research Institute Company Limited, Beijing 100027, China


More Information
Corresponding author: SUN JianGuo,E-mail:sun_jg@jlu.edu.cn
MSC: P631,P738

--> Received Date: 02 February 2018
Revised Date: 13 July 2018
Available Online: 05 September 2018


摘要
零炮检距数据在海洋地震资料处理中有很多优势和用途,然而,受海洋水平拖缆地震采集作业方式的限制,接收数据的最小炮检距一般在200 m左右,小于该炮检距的数据是无法直接获得的.通常的做法是通过对较大炮检距数据进行动校,通过外推来变相获得零炮检距(包括小炮检距)数据,其外推的精度会受到地震资料信噪比、动校正速度的精度等因素影响,并且保幅性较差.本文通过一种基于Kirchhoff真振幅偏移和反偏移串联的技术,在反偏移过程中改变观测系统,有效实现了大炮检距反射地震数据向零炮检距(包括小炮检距)数据之间的转换,且很好地保持了零炮检距(包括小炮检距)数据的振幅特性.同时,经偏移-反偏移串联处理后,有效压制了地震数据中的随机噪声,地震资料信噪比和成像精度均得到显著提高.
零炮检距/
真振幅/
偏移/
反偏移/
数据变换

Zero offset data has many advantages and applications in marine seismic data processing. However, limited by the marine streamer seismic acquisition method, the minimum offset of received data is generally about 200 meters, and the data with offset smaller than it cannot be obtained directly. The usual approach to get the zero offset data (including small offset data) is by extrapolating larger offset data after NMO correction. Unfortunately, the accuracy of this extrapolation is affected by the signal-to-noise ratio of seismic data and the accuracy of velocity for NMO correction, and this method is difficult to preserve the true amplitude. In this paper, based on the Kirchhoff true-amplitude migration and demigration series technique, in which the observation system is changed during the process of demigration, the zero-offset (including small-offset) data are converted from the large offset seismic data effectively while the amplitude characteristics data are preserved. In addition, after the series processing of migration and demigration, the random noise in seismic data is effectively suppressed and the signal-to-noise ratio and the imaging precision of seismic data are significantly improved.
Zero-offset/
Kirchhoff/
True-amplitude/
Demigration/
Observation system



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