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Anisotropic PP and PSv Prestack Depth Imaging of 4C Data, Pamberi, Offshore Trinidad

机译:各向异性PP和PSv 4C数据的叠前深度成像,特立尼达,潘贝里

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In 2004, EOG Resources acquired an OBC 4C swath survey across the Pamberi-1 well location in the Columbus basin, eastern offshore Trinidad. Details of the P- and PSv-wave processing through anisotropic PrSTM were previously described (Johns et al., 2006) in which it was demonstrated there existed a qualitative correlation between derived parameters and attributes from P and Sv anisotropic migration velocities and regional geology. Under the “Future work” section of the previous publication, it was suggested that further data quality enhancement, in preparation for more quantitative rock property classification, could only be achieved from PrSDM imaging. In this paper, we present that next phase in the 4C processing, advancing the P- and PSv-wave data through anisotropic PrSDM, using cell-based tomography with a top-down layer-stripping approach. The Pamberi-1 well was used to initially constrain the anisotropy in the shallow section, with the deeper, spatial trend away from the well determined from the anisotropy derived previously in the time processing, later refined from event registration. Prior to the anisotropic PrSDM, the magnitude of shear splitting from the presence of azimuthal anisotropy is first examined to assess its potential impact on the PS data quality.
机译:2004年,EOG Resources在特立尼达东部沿海哥伦布盆地的Pamberi-1井位获得了OBC 4C测绘带测量结果。先前已经描述了通过各向异性PrSTM进行的P波和PSv波处理的细节(Johns等人,2006年),其中证明了从P和Sv各向异性迁移速度以及区域地质学得出的参数与属性之间存在定性关联。在先前出版物的“未来工作”部分中,建议仅通过PrSDM成像才能进一步提高数据质量,以进行更定量的岩石属性分类。在本文中,我们介绍了4C处理的下一阶段,即使用基于细胞的层析成像和自上而下的层剥离方法,通过各向异性PrSDM推进P波和PSv波数据。 Pamberi-1井最初用于约束浅层剖面中的各向异性,而较深的空间趋势则远离由先前在时间处理中得出的各向异性所确定的井,后来又从事件配准中得到了完善。在各向异性PrSDM之前,首先要检查由于方位各向异性的存在而产生的剪切分裂幅度,以评估其对PS数据质量的潜在影响。

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