常规叠后地震道反演技术，受多种因素的影响。
Routine post-stack seismic trace inversion techniques are affected by many factors.
利用平湖八角亭工区的近中远角道集数据体，成功应用了同时反演算法（SADI），最终将地震振幅数据体转化为描述岩石岩性和流体的属性数据体。
SADI algorithm was executed successfully in the BJT area with near-, middle-, and far-stack dataset, and amplitude dataset was finally converted to attributes dataset describing lithology and fluid.
本文提出了由井旁道出发逐道进行的叠后地震剖面的线性化波阻抗反演方法。
We put forward the linearized wave impedance inversion which, starting from borehole-side trace, is performed trace by trace in a stacked seismic section.
目前常规的叠后地震反演主要包括道积分，递推反演，基于模型反演，但这些反演都是反演波阻抗具有局限性。
At present regular post-stack seismic inversion include recursive inversion, model inversion seismic which are impedance inversion and have their limitations.
目前常规的叠后地震反演主要包括道积分，递推反演，基于模型反演，但这些反演都是反演波阻抗具有局限性。
At present regular post-stack seismic inversion include recursive inversion, model inversion seismic which are impedance inversion and have their limitations.
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