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应用地球物理  2010, Vol. 7 Issue (2): 135-142    DOI: 10.1007/s11770-010-0237-1
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弱各向异性介质中P-SV波弹性阻抗与流体识别因子
崔杰1,韩立国1,刘前坤2,张显文1,韩利1
1. 吉林大学 地球探测科学与技术学院,长春 130026
2. 中国国土资源航空物探遥感中心,北京 100083
P-SV wave elastic impedance and fluid identification factor in weakly anisotropic media
Cui Jie1, Han Li-Gguo1, Liu Qian-Kun2, Zhang Xian-Wen1, and Han Li1
1. College of Geo-Exploration Science and Technology, Jilin University, Changchun 130026, China.
2. China Aero Geophysical Survey and Remote Sensing Center for Land and Resources, Beijing 100083, China.
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摘要 基于Petr Jilek正交各向异性介质中的P-SV波反射系数精确公式,将其退化到VTI和HTI介质中,得到了保留到 三次幂的近似公式,同时结合Kenneth横波弹性阻抗原理,推导建立了VTI和HTI介质中P-SV波的弹性阻抗近似公式;在此基础上构建了弱各向异性介质中的流体识别因子公式,通过理论模型对Castagna和Smith的岩性组合进行了识别;最后详细分析了各向异性参数的取值对P-SV波弹性阻抗及识别因子产生的影响及变化趋势。
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崔杰
韩立国
刘前坤
张显文
韩利
关键词弹性阻抗   流体识别因子   各向异性参数   VTI   HTI     
Abstract: The P-SV wave reflection coefficients in VTI and HTI media were obtained by approximation of the Jilek (2002a and b) equation in orthotropic anisotropic media. An approximate equation for P-SV wave elastic impedance can be derived from the combination of the new coefficients with S-wave elastic impedance (Duffaut et al., 2000). On this basis, the fluid identification factor in weakly anisotropic media was constructed and used to identify the Castagna and Smith (1994) lithologic combination and achieved good results. Finally, we specifically analyzed the anisotropic parameter impacts P-SV wave elastic impedance and fluid factor trends. 
Key wordsP-SV wave elastic impedance   fluid identification factor   anisotropic parameter   VTI   HTI   
收稿日期: 2009-12-15;
基金资助:

本研究由国家973计划“保持动力学特性的地震成像方法课题(2007CB209603)”子课题资助。

引用本文:   
崔杰,韩立国,刘前坤等. 弱各向异性介质中P-SV波弹性阻抗与流体识别因子[J]. 应用地球物理, 2010, 7(2): 135-142.
CUI Jie,HAN Li-Guo,LIU Qian-Kun et al. P-SV wave elastic impedance and fluid identification factor in weakly anisotropic media[J]. APPLIED GEOPHYSICS, 2010, 7(2): 135-142.
 
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