Application of the AVO gradient-based spectral bluing technique in the characterization of thin sandstones in moderately deep strata
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摘要: 传统谱蓝化主要用于叠后地震拓频处理,适用于测井波阻抗能较好辨别砂、泥岩的浅层,对于中深层阻抗混叠区局限性较大。AVO梯度反映相对反射系数随炮检距的变化,与泊松比变化率呈现正相关,而泊松比能较好辨别中深层砂、泥岩。本文首先通过岩性组合、物性及流体等参数变化,正演论证了AVO梯度在中深层辨识砂岩顶界面的可靠性与稳定性;进一步地,针对中深层薄砂岩刻画精度低问题,提出一种基于AVO梯度信息的谱蓝化地震拓频技术,通过对AVO梯度谱蓝化拓频,提高薄储层刻画精度。模型试算及实际应用表明:基于AVO梯度的谱蓝化可以直接运用AVO梯度辨识储层界面信息,简化基于CRP道集或角度部分叠加的多参数岩性预测方法;同时,该方法较好解决了XH凹陷深埋地层薄砂岩刻画难题,对中深层地震高分辨率处理有一定借鉴意义。Abstract: The conventional spectral bluing technique is mainly utilized for post-stack seismic frequency expansion.It is applicable to the shallow strata where sandstones and mudstones can be effectively identified based on the wave impedance of logs.However,this technique has many limitations for the impedance aliasing zones of moderately deep strata.The amplitude versus offset (AVO) gradient reflects the change in the relative reflection coefficient with offset and is positively correlated with the rate of change in Poisson's ratio,which can distinguish between sandstones and mudstones in moderately deep strata.Through forward modeling,this study first proved the reliability and stability of the AVO gradient in identifying the top interface of sandstones in moderately deep strata according to the changes in parameters such as lithologic association,physical properties,and fluids.Furthermore,to improve the characterization precision of thin sandstone interbeds in moderately deep strata,this study proposed a AVO gradient-based spectral bluing for seismic frequency expansion.The model tests and practical applications show that the spectral bluing based on AVO gradient can directly identify the information on reservoir interfaces and simplify the multi-parameter lithology prediction method based on CRP gathers or partial angle stack data.Moreover,the new technique proposed in this study can effectively characterize the thin sandstones in deeply buried strata in the XH sag and provides a reference for high-resolution seismic processing of moderately deep strata.
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