中文摘要：

天然气水合物稳定带下方游离气分布模式、气体含量及其对水合物富集成藏的指示是水合物研究中的难点,而利用振幅随偏移距变化（Amplitude Versus Offset,AVO）与岩石物理模型能够对游离气含量进行地震定量解释.我们对印度Krishna-Godavari（K-G）盆地的地震资料进行了叠前保幅处理,在测井数据和层位标定的基础上,基于等效介质岩石物理模型和AVO正演模拟定量估算了NGHP01-10A井的游离气饱和度,发现水合物下方的游离气饱和度与其分布模式有关.游离气呈均匀分布时饱和度为孔隙空间的0.3%~0.4%,而块状分布时为3%~4%,该结果与NGHP01-10D实测计算的泊松比交汇分析结果吻合很好.最后再根据干燥岩石骨架的泊松比反演结果进一步判断游离气分布为均匀分布,其饱和度为0.3%~0.4%.

英文摘要：

Distribution,saturation and hydrate indicator of free gas beneath gas hydrate stability zone have been the difficulty in the research of gas hydrate.Amplitude versus offset（AVO）and rock physics can be used to quantitatively interpret free gas saturation.In this paper,seismicdata,acquired at K-G basin,India,have been processed to preserve true amplitude information.Based on the logging data and horizon calibration,free gas saturation of NGHP01-10 Ais assessed with effective medium theory and AVO modeling.It is found that free gas saturation is related to its distribution patterns. Assessments of free gas saturation in homogeneous and patchy distribution are 0.3% ～0.4% and 3% ～4%,respectively.The results show good agreement with the crossplot of Poisson′s ratio which are calculated by the measurement at NGHP01-10 D.Free gas is further deduced to be homogeneous distribution on the base of dry matrix Poisson′s ratio with the saturation of 0.3%～0.4%.