新疆石油地质 ›› 2011, Vol. 32 ›› Issue (6): 660-663.

• 应用技术 • 上一篇    下一篇

三维转换波静校正技术

宋玉梅   

  1. 中国石油大庆油田有限责任公司勘探开发研究院,黑龙江大庆 163712
  • 收稿日期:2011-03-30 出版日期:2011-12-01 发布日期:2020-08-20
  • 作者简介:宋玉梅(1961-),女,山东龙口人,工程师,地球物理勘探,(Tel)0459-5508738(E-mail)ymsong@petrochina.com.cn.

Static Correction Technique for 3D Converted Wave

SONG Yu-mei   

  1. Research Institute of Exploration and Development, Daqing Oilfield Company Ltd., Daqing, Heilongjiang 163712, China
  • Received:2011-03-30 Online:2011-12-01 Published:2020-08-20

摘要: 利用大庆油田喇嘛甸区块三维三分量地震数据,依据静校正量由大到小分层次解决的思路,首先采用模型法解决了与基准面有关的长波长静校正分量问题,然后在共检波点叠加剖面上利用纵波和转换波的反射信息解决中长波长静校正分量问题,最终应用地表一致性剩余静校正解决短波长静校正分量问题。实际应用结果表明,喇嘛甸区块三维转换波成像剖面与纵波剖面在构造、断层上的形态一致,而且波组保持了纵、横波各自的特点,为后续利用纵、横波联合进行储集层物性分析奠定了基础。

关键词: 三维转换波, 静校正量, 表层模型, 共检波点叠加, 剩余静校正, 纵横波联合

Abstract: The static correction of converted wave is far complicated than that of P-wave, and it directly influences the imaging quality of the converted wave. On the basis of 3D3C seismic data in Lamadian studied area, the statics are corrected via step-by-step solution from large to small of statics. The model method is firstly adopted to solve the problem of the static component of the long wave length related with the datum level, and then by using the reflection information of P-wave and converted wave on common receiver stack profile, the medium-long wave length can be dealt with. Finally, the same task for the short wave length can be also completed through surfaceconsistent residual static correction. The practical results show that the 3D converted wave imaging profile in Lamadian studied area is accordant with the P-wave profile in styles of structure and fault, furthermore, the wave group sustains the individual characteristics of Pwave and S-wave, thus the above achievements have laid the foundation of the petrophysical property analysis of the reservoirs using Pwave and S-wave combination.

Key words: 3D converted wave, statics, surface model, common receiver stack, residual static correction, P-wave and S-wave combination

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