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厚风化层覆盖区转换波静校正方法
引用本文:李彦鹏,马在田,孙鹏远,杨海申.厚风化层覆盖区转换波静校正方法[J].地球物理学报,2012,55(2):614-621.
作者姓名:李彦鹏  马在田  孙鹏远  杨海申
作者单位:1. 同济大学海洋与地球科学学院, 上海 200092; 2. 东方地球物理公司, 河北涿州 072750
摘    要:P-SV转换波处理与传统的P-P波处理有很大的不同,如S波静校正、CCP叠加、P-SV速度分析和偏移等,其中最大的难题就是S波静校正问题.S波速度基本不受潜水面的影响,与纵波静校正没有直接相关性,有时横波静校正量能达到纵波静校正量的十倍,用纵波静校正量乘以比例系数来解决横波静校正问题将导致较大误差.同一接收点X和Z分量存在一定的初至时差,该时差代表了P波和S波在低降速带的走时差,可以利用该时差和近地表纵横波速度比信息去除低降速带对横波的影响,得到准确的静校正量.本文利用多分量初至时差推导了较为精确的横波静校正公式,再结合共检波点叠加求取剩余静校正量的方法,形成了完整的转换波静校正配套方法.利用该方法对苏里格气田二维及三维多波地震资料进行了实际处理,数据处理结果证明了该方法的有效性,该方法尤其适用于其他方法难以奏效的风化层较厚地区的横波静校正量求解,该方法也同时考虑了长波长横波静校正问题.

关 键 词:转换波  横波  静校正  初至时差  
收稿时间:2011-07-19

Converted-wave static correction method for thick weathering area
LI Yan-Peng , MA Zai-Tian , SUN Peng-Yuan , YANG Hai-Shen.Converted-wave static correction method for thick weathering area[J].Chinese Journal of Geophysics,2012,55(2):614-621.
Authors:LI Yan-Peng  MA Zai-Tian  SUN Peng-Yuan  YANG Hai-Shen
Institution:1. School of Ocean and Earth Science, Tongji University, Shanghai 200092, China; 2. BGP Inc., Zhuozhou Hebei 072750, China
Abstract:In P-SV seismic data processing,there are some aspects different from conventional P-P seismic data processing,such as S-wave static correction,CCP binning,P-SV velocity analysis and migration.Among them,the most difficult procedure is S-wave static correction.Unlike P-wave velocity,the S-wave velocity is almost unaffected by the water table and generally very low.Hence,the P-wave and S-wave static solutions are largely different from each other,sometimes S-wave statics are near ten times of P-wave′s.So the approximation of the S-wave statics by simply scaling the known P-wave statics will lead to large errors and a good image can not be obtained.It has been proven that the time difference of first break between X and Z component in same receiver represents the travel time difference of P-and S-wave in weathering layer and it can be utilized to calculate S-wave statics.This paper presents an accurate statics expression with respect to the time difference of first break and some velocity ratio parameter of near surface.Combined with residual statics estimated from common receiver stack section,an integrated converted-wave static correction method has been presented.The method was applied to 2D-3C and 3D-3C data processing of Shulige gas field.The results show a good image which indicates that this method is effective for P-SV data processing.This method is especially suitable for statics estimation of thick weathering area where other methods are disabled.Long period S-wave statics are considered simultaneously.
Keywords:Converted-wave  Shear-wave  Static correction  Time difference of first break
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