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Conditioning Prestack Seismic Data in the Offset-azimuth Domain

机译:在偏移方位角域中调节叠前地震数据

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These days acoustic and elastic impedance are commonly derived from 3-D seismic data, which help us compute porosity and reservoir fluid estimates. Somewhat less commonly, vertical fracture density and fracture orientation in the reservoir rocks are derived from seismic data, enhancing our ability for optimum placement of horizontal wells and optimal recovery. To achieve the latter objective, good quality seismic data are required, which might be acquired not only with such objectives in mind, but also to yield data with good signal-to-noise ratio. The processing sequence adopted for the seismic data employs all the usual steps, including 5-D interpolation used for regularization of the offset and azimuth sampling within common mid-point, or CMR gathers. Thereafter, the common procedure is to azimuthally sector the gathers (six sectors of 30 degrees each), and put them through the azimuthal amplitude variation with offset, or AVO, analysis procedure to determine the fracture density and orientation.
机译:如今,声阻抗和弹性阻抗通常来自3-D地震数据,可帮助我们计算孔隙率和储层流体估算值。不太常见的是,储层岩石中的垂直裂缝密度和裂缝方向是根据地震数据得出的,从而增强了我们优化水平井和优化采收率的能力。为了实现后一个目标,需要高质量的地震数据,不仅要牢记这些目标,而且要获得具有良好信噪比的数据。地震数据所采用的处理顺序采用所有常规步骤,包括用于对中点或CMR采集内的偏移量和方位角采样进行正则化的5-D插值法。此后,通常的步骤是对聚拢物进行方位扇形(每个扇形为六个扇形,每个扇形为30度),然后对它们进行带有偏移量或AVO的方位角振幅变化分析程序,以确定裂缝的密度和方向。

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    《AAPG Explorer》 |2019年第10期|18-19|共2页
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