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Factors of effect on accuracy of velocity field in south edge of Tianshan and its effect on depth imaging

机译:影响天山南缘速度场精度的因素及其对深度成像的影响

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摘要

We design the seismic geological model in the area of the south edge of Tianshan which includes a shallow conglomerate layer with high velocity of group Xiyue of Quaternary at the north of Yaken, and a low velocity gypsum-rock layer whose structure varies widely in a deep layer of group Jidieke of Tertiary. The shot gathers are synthesized based on the field observation system. Then stacking velocities (Vs) and a migration section are obtained and Vs is compared with the actual root-mean-square velocity (Vrms) of the model. The results show that Vs is smaller than the actual Vrms when the velocity varies laterally over the target layer. Vs can also be larger than the actual Vrms due to a shallow conglomerate. As a result of the synthetic effect, Vs is 8% larger than the actual Vrms. Moreover, the shallow high velocity conglomerate slightly affects the time image of deep layers, but the Vs of the deep layers at two ends of the conglomerate is increased, which results in the false synclines in deep layers and enlarges the height of the structure near the synclines.
机译:我们在天山南缘地区设计了地震地质模型,该模型包括位于雅肯北部第四纪第四系西岳群高速的浅层砾岩层,以及在深部构造差异很大的低速石膏岩层。第三层基迪克组。基于野外观察系统,合成了炮弹。然后获得叠加速度(Vs)和迁移截面,并将Vs与模型的实际均方根速度(Vrms)进行比较。结果表明,当速度在目标层上横向变化时,Vs小于实际Vrms。由于结块较浅,Vs也可能大于实际Vrms。由于合成效应,Vs比实际Vrms大8%。此外,浅层高速砾岩对深层的时间图像影响较小,但砾岩两端的深层的Vs增大,这导致深层的假向斜,并增大了近地层的结构高度。同步线。

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