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3D Post-Stack Acoustic Impedance Inversion Results for Kijing and Malong Fields,South Natuna Sea

机译:南纳图纳海Kijing和Malong油田的3D叠后声阻抗反演结果

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Post-stack acoustic impedance inversion was performed atKijing, Malong, and Buntal fields. The results allow detailedreservoir characterization of the fields to be done, and predictthe location of porous, reservoir-quality sands, and in manycases, reservoir-quality sands that contain gas. Several aspectsof the inversion results prove to be useful that cannot beachieved through the use of seismic analysis alone. Theremoval of wavelet effects (tuning, extra events due toconstructive wavelet sidelobe interference, and dimming dueto destructive wavelet sidelobe interference) is one importantenhancement. Seeing the impedances as layer propertiesinstead of as interfaces allows information about the sands andshales to be observed. Increase in bandwidth, both on the lowend with the introduction of a good low frequency model fromthe interpolation/extrapolation of well log impedance alonginterpreted horizons and the use of geologic constraints, andon the high end due to the use of a spectral whiteningdeconvolution operator and proper inversion parametersproduces increased resolution.The inversion results at Kijing, Malong, and Buntal fields maybe used to discern details about the reservoir sands, especiallyin conjunction with the current geologic and geophysicalinformation from conventional seismic data, well logs,analogs, etc. 3D visualization of the reservoir shows thestructure of the sands, most of which are channelized.
机译:叠后声阻抗反演在 Kijing,Malong和Buntal字段。结果允许详细 对要完成的油田进行储层表征,并进行预测 多孔的,储层质量的砂的位置,以及在许多地方 在这种情况下,储层质量的砂子中含有气体。几个方面 反演结果证明是有用的,不能 仅通过地震分析即可实现。这 去除小波效应(调整,由于 相长小波旁瓣干扰和调光 破坏性小波旁瓣干扰)是重要的 增强。将阻抗视为层属性 而不是作为接口允许有关沙子和沙子的信息 页岩要观察。带宽增加,两者都低 最后引入了一个很好的低频模型 沿测井阻抗的内插/外推 解释层位和地质约束条件的使用,以及 由于使用了光谱增白,因此在高端 反卷积算子和适当的反演参数 产生更高的分辨率。 Kijing,Malong和Buntal油田的反演结果可能 用于识别有关储层砂的细节,尤其是 结合当前的地质和地球物理 来自常规地震数据,测井的信息, 类似物等。储层的3D可视化显示 沙的结构,其中大多数是带槽的。

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