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首页> 外文期刊>Journal of Petroleum Science & Engineering >Enhanced compartmentalization of a complex reservoir with sub-seismic faults from geological inversion
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Enhanced compartmentalization of a complex reservoir with sub-seismic faults from geological inversion

机译:具有地质反演的亚地震断层的复杂油藏的分隔性增强

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摘要

Sealing faults are fundamental for delimitation of compartments in a reservoir and they are usually identified by geological interpretation of 3D seismic data which are limited to the resolution of seismic sections: Dynamic production data may suggest in some cases the existence of smaller faults or vertical discontinuities which may not be detected from seismic. It is reasonable to assume that, with increasing resolution of 3D seismic, large faults could be accurately identified while faults with strike slip or small throw may remain invisible to seismic. This paper proposes a geological inversion approach for modeling sub-seismic vertical discontinuities or faults using dynamic data. The methodology is based on a prior self-similar generation of faults which are geometrically downscaled from larger faults interpreted from seismic. Then, the approach follows an iterative inverse Gauss-Newton modeling technique to update fault size and location parameters based on the reservoir pressure response. The convergence criteria include comparing both the observed and model calculated shut-in bottom-hole pressure (SBHP) and flowing well head pressure (FWHP) until the squared differences between the observed and model calculated pressures diminish to a minimum. If the convergence criteria were not met, the fault pattern is modified and the geocellular grid is cut with updated faults to generate a new version of the faulted simulation model for the next iteration. As an alternative, commercial assisted history match (AHM) software can be utilized to expressively adjust fault locations in the simulation model to match the production history; however, such perturbations are not done at the geological level as in the proposed approach. Thus, the approach in this paper has the advantage of preserving the spatial and geological integrity of the geocellular model. In addition, the spatial consistency between the geological and simulation models is always guaranteed in the proposed approach.
机译:密封断层是界定储层隔层的基础,并且通常通过对3D地震数据进行地质解释来识别,而这些地震数据仅限于地震剖面的解析:动态生产数据在某些情况下可能表明存在较小的断层或垂直不连续性,可能无法从地震中检测到。合理地假设,随着3D地震分辨率的提高,可以准确地识别出大断层,而具有走滑或小倾角的断层可能仍对地震不可见。本文提出了一种利用动态数据对亚地震垂直不连续性或断层进行建模的地质反演方法。该方法基于先前的自相似断层生成,这些断层从地震解释的较大断层几何缩小。然后,该方法遵循迭代逆高斯-牛顿建模技术,以基于储层压力响应来更新断层大小和位置参数。收敛标准包括比较实测和模型计算的封闭井底压力(SBHP)和流动井口压力(FWHP),直到实测和模型计算的压力之间的平方差减小到最小。如果不满足收敛标准,则修改断层图样,并用更新后的断层切割地蜂窝网格,以为下一次迭代生成新版本的断层仿真模型。作为替代,可以使用商业辅助历史匹配(AHM)软件来表达性地调整仿真模型中的故障位置以匹配生产历史。但是,这种扰动并没有像建议的方法那样在地质层次上发生。因此,本文中的方法具有保持地质细胞模型的空间和地质完整性的优势。此外,在所提出的方法中始终保证了地质模型和模拟模型之间的空间一致性。

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