收稿日期: 2005-12-26
修回日期: 2006-02-19
网络出版日期: 2006-04-20
THE APPLICATION OF 3D CONVERTED WAVE FIRSTBREAK REFRACTION STATIC IN THE SLG AREA
Received date: 2005-12-26
Revised date: 2006-02-19
Online published: 2006-04-20
王宇超;牛滨华;张年春;马龙;王建华; . 转换波三维初至静校正方法在SLG气区的应用[J]. 天然气地球科学, 2006 , 17(2) : 272 -275 . DOI: 10.11764/j.issn.1672-1926.2006.02.272
Due to converted shear wave have lower velocity than P wave and the fluid in the medium have no action to converted shear wave. The near surface model for conve rted shear wave is different from that for P wave. The static of converted shear wave become more important and serious than P wave in converted shear wave seis mic data processing. In this article,first,use firstbreak time of P wave to ob tain the near surface model;second,pick the firstbreak time difference between P wave and converted shear wave by cross correlation;then,calculate the stati c of converted shear wave.We use the real 3D converted wave seismic data in the SLG area. As it shows in this paper, the problem of converted shear wave stati c is solved perfectly.We suggest that this method may be widely used in convert ed shear wave seismic data processing.
[1 ] 牛滨华,孙春岩.半空间介质与地震波传播[M].北京:石油工业出版社 ,2002.
[2] 刘全新,李道善.关于山地静校正和偏移基准面的一些认识 [J ].天然气地球科学, 2003,14(1):57-59.
[3 ] 詹正彬,姚姚.多分量地震和横波勘探[M].北京:地质出版社,1993.
[4 ] 张树林,夏斌,何家雄.海上多波多分量地震采集技术的应用——以莺歌海盆地为例 [J ].天然气地球科学,2005,16(1):103-107.
[5] CARY P W, EATON D W S.A simple method for resolving large converted-wave (P-SV)statics[J].Geophysics, 1993,58(3):429-433.
[6] 唐建侯,张金山.消除P-SV波大静校正量的方法[J].石油地 球物理勘探,1994,29(5):650-653.
[7] 李彦鹏,谷跃民.利用上行透射转换波计算横波静校正量 [C ]//国际地球物理会议论文集,CPS/SEG,2004:114-116.
/
| 〈 |
|
〉 |