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Using 3D4C Data to Image and Interpret theSeismically Obscured Area over the TommelitenAlpha Discovery

机译:在TommeliteNalpha Discovery中使用3D4C数据来图像并解释宗旨遮挡区域

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Ahigh density 3D4C seismic survey was acquired over the TommelitenAlpha gas condensate discovery in2005 to image a seismically obscured area caused by complex velocity and density variations in theoverburden. Both full azimuth PP and PS data were used and pre-stack co-depth migrated. The result wasan improved image of the previously obscured area, especially in the PS dataset. The size of theSeismically ObscuredArea (SOA) was reduced also in the pre-stack depth migrated PP data, but in thisouter part of the SOAthe PP data gave a different image compared to the PS dataset - making theinterpretation challenging.Although the resolution of the PS data is lower at the target level, and the mainEkofisk Fm reservoir target (21-24m thick) is below PS seismic resolution, the PS dataset proved veryuseful in mapping the structural shape and faults inside the SOA, leaving only a small central areaobscured.
机译:在TommeliteNalpha气体冷凝物发现中获得了高密度3D4C地震测量,以In2005获得由Theoverbanden的复杂速度和密度变化引起的地震遮光区域。使用全方位角PP和PS数据并使用预堆叠共迁移。结果是改进了先前模糊区域的图像,特别是在PS数据集中。在堆叠预堆叠深度迁移的PP数据中也减少了默认的lemuredAlea(SOA)的大小,但是,与PS数据集相比,SOAthe PP数据的部分地产生了不同的图像 - 使Interpretation Colleging。尽管PS的分辨率数据在目标级别较低,并且MaineKofisk FM水库目标(21-24M厚)低于PS地震分辨率,PS数据集证明了绘制了SOA内部结构形状和故障,仅留下了一个小中心区域。

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