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用非零偏P-P波、P-SV波计算零偏反射纵波和反射横波
引用本文:张宝金,成谷,曹景忠,马在田,许世勇. 用非零偏P-P波、P-SV波计算零偏反射纵波和反射横波[J]. 地球物理学进展, 2002, 17(1): 102-106
作者姓名:张宝金  成谷  曹景忠  马在田  许世勇
作者单位:同济大学教育部海洋地质重点实验室,上海,200092
基金项目:国家自然科学基金项目 (4 9894190 2 8)
摘    要:在P波入射时,地下同一点产生的P-P波和P-SV波是入射角、界面两侧纵波阻抗和横波阻抗的函数,并且两者是耦合的,利用两者的耦合关系,可在入射角确定的情况下提取与入射角无关的零偏纵波反射和横波反射。本文对此进行了理论推导,结论是:入射角为零时的纵波与横波反射系数是入射角非零时的P-P波和P-SV波反射系数的线性组合,进而可以用纵横波反射计算泊松比反向间面,把多波叠前反演转化到叠后进行,通过合成弹性参数反射剖面,直接反演弹性参数等,都很有意义。文中给出了有关的公式,并对具体实现方法和有关参数进行了讨论。

关 键 词:转换波 反演 岩性 反射地震勘探 非零偏P-P波 P-SV波 零偏反射纵波 反射横波
文章编号:1004-2903(2002)01-0102-05
修稿时间:2000-05-13

Calculating the Zero Offset P and S Reflection Using the Nnoe-Zero Offset P-P and P-SV Wave
ZHANG Bao-jin CHENG Gu CAO Jing-zhong MA Zai-tian XU Shi-yong. Calculating the Zero Offset P and S Reflection Using the Nnoe-Zero Offset P-P and P-SV Wave[J]. Progress in Geophysics, 2002, 17(1): 102-106
Authors:ZHANG Bao-jin CHENG Gu CAO Jing-zhong MA Zai-tian XU Shi-yong
Abstract:When P wave incidents,The P-P wave and P-SV wave created from the same point are both functions of incidence angle,and of the media above and below the interface,V p and V s they are coupled.Using this kind of coupled relationship,the zero-offset P wave reflection and S wave reflection,which don't depent on the incidence angle,can be obtained with the incidence angle determined,In this paper the theoretical deduction is carried out and the following concusion is obtained:the reflection coefficient of P wave and S wave when the incidence angle is zero is the linear combination of with none-zero incidence angle.Furthermore,the reflection of Poisson's can be calculated using P wave and S wave reflection.They are all meanjngful to transform the multi-wave prestack inversion into poststack,and directly invert elastic parameters.In the paper,the implementatio methods and the relative formulation are also discussed.
Keywords:AVO  Converted wave  Inversion  Lithology  
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