塔里木盆地轮南地区三叠系非均质薄砂岩储层预测

    Prediction of heterogeneous,thin Triassic sandstone reservoirs in the Lunnan area,Tarim Basin

    • 摘要: 塔里木盆地轮南地区三叠系整体为陆相三角洲沉积体系,研究区内发育有三角洲平原、三角洲前缘和前三角洲等亚相,储层相变快,砂泥岩高频交互沉积,导致储层薄、非均质性强,为高精度储层预测带来极大困难。为此,本文以沉积岩石学、地震层序地层学为指导,开展地震、地质综合研究,并以等时层序解释为基础,结合地震相分析成果,建立岩相模型,约束叠前地质统计学反演过程,落实砂体空间展布特征。实际应用表明,该方法在提高非均质薄储层纵向分辨能力的同时,大幅降低了横向不确定性,预测结果与井上实钻及生产动态数据相吻合,可为油气藏高效开发提供支撑。

       

      Abstract: The Triassic strata in the Lunnan area of the Tarim Basin represent a continental deltaic sedimentary system,with sedimentary subfacies including deltaic plain,deltaic front,and prodelta.The rapid phase transition of reservoirs and the high-frequency sand-mudstone alternating deposition create thin,highly heterogeneous reservoirs,rendering high-precision reservoir prediction extremely challenging.Under the guidance of sedimentary petrology and seismic sequence stratigraphy,this study conducted comprehensive seismic and geological research.Then,based on isochronous sequence interpretation,as well as seismic facies analytical results,this study established a lithofacies model.By constraining the pre-stack geostatistical inversion process,this study determined the spatial distribution of sand bodies.The practical application demonstrates that the proposed method enhances the vertical resolution of heterogeneous,thin reservoirs while significantly reducing lateral uncertainty.The predicted results align with actual drilling and production performance data and thus can provide valuable support for the efficient exploitation of hydrocarbon reservoirs.

       

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