用AVO方法从定性到半定量检测砂岩含气性

2005年 12卷 第01期
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Detect the Gas Bearing Propertics of Sandstone
Using AVO Method—from Qualitatively Interpretation
to Ha lf-quantitatively In terpertation
 贺保卫1 潘仁芳2 莫午零2 刘亚明2
东方地球物理公司研究院敦煌分院 长江大学地球科学学院
   介质的孔隙度、含气饱和度等是影响地震波振幅随炮检距变化的重要因素。在已知含气饱和度和泊松比变化关系的基础上,应用Wyllie公式,对不同孔隙度情况下的砂岩介质做变含气饱和度正演模型研究,并通过P、G交会图分析它们的AVO响应特征,使以往的AVO定性解释变为半定量化,从而更好地为AVO反演服务。

The Porosity and fluid saturate are the singificant factors

that effect on amp litude variation with offset of seismic wave

in the medium. Based on the kmown relationship of the

Poisson ratio and gas saturate, we imitate different fluid

saturation AVO models in sandstone which has different

porosity usingWyllie formula and analyze those parameters to

know how they affect AVO attributive parameter using PG

cross p lot in this paper , which change AVO qualitatively

interp retation to half quantiatively in order to give better

service forAVO interpertation .

AVO; 孔隙度; 含气饱和度; 正演模型;

AVO , Porosity, Fluid saturate, Forward

model.

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