川北元坝地区致密砂岩储层天然裂缝特征

Yanqing Huang , Ruyue Wang
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引用次数: 1

摘要

天然裂缝对于致密砂岩气藏的高产、稳产具有重要意义。然而,由于非均质性强,通常很难准确表征致密砂岩气藏中它们的分布。采用岩心描述、测井解释和地震预测相结合的方法,对四川盆地元坝地区须家河组致密砂岩气藏天然裂缝进行了综合表征。研究结果表明:(1)须家河组天然裂缝以低角度裂缝为主,少量中、高角度裂缝。裂缝发育程度主要受距断层距离、地层弯曲程度和岩石力学层厚度的控制。(2) 以优选最大似然、结构熵、基于光源的对称性和高精度曲率等裂缝敏感地震属性为输入,应用基于贝叶斯概率模型的无监督聚类分析算法预测不同倾角下大规模裂缝的分布;在窄方位叠前CMP道集优化的基础上,采用Hampson-Russel的ProAZ全CMP道集各向异性检测技术,对中小尺度裂缝的分布进行了表征,预测的裂缝发育强度与成像测井的裂缝解释结果匹配85%以上。此外,预测的裂缝方向与成像测井基本一致。(3) 徐家河组断裂成因断裂主要分布在九龙山背斜东南侧断裂附近,呈NE向窄条带分布。褶皱成因断裂主要发育于徐三段,位于九龙山背斜轴线及其东南侧,地层弯曲强烈。该研究为致密砂岩气藏的开发提供了坚实的基础,并扩展了裂缝精确表征的方法。
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Characterization of natural fractures in tight sandstone reservoirs in Yuanba area, northern Sichuan Basin

Natural fractures are quite important for the high and stable production of tight sandstone gas reservoirs. However, it is commonly difficult to accurately characterize their distribution in tight sandstone gas reservoirs due to the strong heterogeneity. A comprehensive characterization of natural fractures in tight sandstone gas reservoirs of the Xujiahe Formation in the Yuanba area, Sichuan Basin, was carried out by multimethod of core description, log interpretation and seismic prediction. The results show that (1) the natural fractures in the Xujiahe Formation are mainly low-angle fractures, with a few medium- and high-angle fractures. The degree of fracture development is mainly controlled by the distance from the fault, the flexural degree of the strata and the thickness of the rock mechanical layer. (2) The fracture-sensitive seismic attributes such as the preferred maximum likelihood, structure entropy, illuminant-based symmetry and high-precision curvature are taken as the input, and the unsupervised cluster analysis algorithm based on Bayesian probability model is applied to predict the distribution of large-scale fractures at different dip angles; on the basis of narrow azimuthal pre-stack CMP gather optimization, the anisotropy detection technique of Hampson-Russell's ProAZ full CMP gather is used to characterize the distribution of small- and medium-scale fractures, and the predicted fracture development intensity matches the fracture interpretation results of the imaging logs by more than 85%. Moreover, the predicted fracture orientation is basically consistent with that of the imaging loggings. (3) The fault-genesis fractures of the Xujiahe Formation are mainly distributed near the fault on the southeast flank of the Jiulongshan anticline, and are distributed in a narrow strip in NE direction. The fold-genesis fractures are mainly developed in the Xu 3rd Member, and are located in the axis of the Jiulongshan anticline and its southeast flank where the strata are strongly flexed. This study provides a solid foundation for the development of tight sandstone gas reservoirs and extends the approaches for the accurate characterization of fractures.

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