摘要
本文从Zoeppritz方程的精确解出发,导出了P-SV波反射系数的高精度近似表达式,证明卜SV波的反射振幅正比于△Vs/Vs。这里,Vs为反财界面两侧横波层速度的平均值;△Vs为两侧横渡层速度的差值。文中将P-SV波共转换点水平叠加改进为共转换点拟合叠加,得到正比于△Vs/Vs的叠加振幅。仿照纵波勘探中的波阻抗技术,利用P-SV波拟会叠加剖面(或其偏移归位剖面)逐层向下递推反演,再加上适当的标定,便可获得横渡层速度剖面。
The desirable approximate expression of P-SV wave refIection coefficient is de-duced from the accurate solution of Zoeppritz's equation. Then,the reflection ampli-tude of P-SV wave is proved to be directly proportional to △Vs/Vs,where Vs is theaverage interval velocity of shear waves at the both sides of reflector,and △Vs is theinterval velocity difference of the shear waves. The horizontal stack of common con-version points of P-SV waves is changed into fitting stack of these comrnon conver-sion points to result in stacked amplitudes which are directly proportional to △Vs/Vs. People can obtain S-wave interval-velocity section by imitating wave impedancetechnique in P-wave exploration,namely,by rnaking downward layer by layer recur-sion inversion and calibration of fitting-stacked (or rnigrated) section of P-SVwaves.
出处
《石油地球物理勘探》
EI
CSCD
北大核心
1995年第1期56-61,共6页
Oil Geophysical Prospecting
基金
国家自然科学基金
中国科学院资助
中国石油天然气总公司资助
大庆石油管理局资助
关键词
叠加剖面
波阻抗
地震勘探
地震波
P-SV wave, stacked section, wave impedance, interval-velocity section