Stratigraphic and structural control over permeability distribution in poorly consolidated siliciclastic rocks

Thayssa Pereira de Andrade, E. V. Barroso, Luis Paulo Vieira Braga, C. L. Mello, J. Souza
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引用次数: 1

Abstract

Permeability models are very relevant for the characterization of oil systems. However, limitations related to the resolution of seismic data make it difficult to identify subseismic, sedimentary, and tectonic structures, which can significantly impact the flow pattern. This study analyzed the spatial variability of permeability according to stratigraphic and structural geology control to propose a useful model for poorly consolidated, fractured, and faulted siliciclastic reservoirs. In an outcrop analogue to this type of reservoir, air permeability was measured in 3 orthogonal directions at 24 points, spaced 2 m apart.The models were obtained by sequential Gaussian simulation (SGS) after statistical data treatment. The models were validated to ensure the consistency of the generated scenarios. Permeability values showed a positive asymmetric distribution and reduced medians toward tectonic structures. The fitted semivariogram model was exponential, with higher spatial continuity in the horizontal flow direction and lower in the vertical one. The permeability models emphasized the importance of considering subseismic structures in the flow analysis of reservoirs since they have proven to play a significant role in the permeability distribution in the outcrop assessed.
地层和构造对弱胶结硅质碎屑岩渗透率分布的控制
渗透率模型与油层系统的表征非常相关。然而,由于地震数据分辨率的限制,很难识别亚地震、沉积和构造构造,而这些构造会对流型产生重大影响。根据地层和构造地质控制,分析了渗透率的空间变异性,提出了一种适用于弱胶结、裂缝性和断裂性硅质碎屑储层的有效模型。在与此类油藏类似的露头中,在3个正交方向上的24个点上测量了空气渗透率,间距为2 m。统计数据处理后,采用序贯高斯模拟(SGS)得到模型。对模型进行了验证,以确保生成场景的一致性。渗透率值呈正不对称分布,中位数向构造方向减小。拟合的半变异函数模型呈指数型,在水平方向上具有较高的空间连续性,在垂直方向上具有较低的空间连续性。渗透率模型强调了在储层流动分析中考虑次地震结构的重要性,因为它们已被证明在评估的露头渗透率分布中起着重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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