南海北部湾盆地涠西南凹陷渐新统涠洲组成岩作用及优质储层预测

    Diagenesis and prediction of high quality reservoirs in the Weizhou Formation of the Oligocene in the Weixinan Sag of the Beibu Gulf Basin, South China Sea

    • 摘要: 为探究南海北部湾盆地涠西南凹陷涠洲组碎屑岩成岩作用及优质储层发育规律,以涠洲X油田涠洲组三段为例,通过薄片鉴定、扫描电镜分析、阴极发光和成岩数值模拟等技术方法,深入分析成岩作用类型及机理、成岩演化序列、成岩相划分,并开展优质储层主控因素分析及优选。结果表明:研究区涠三段储层压实作用中等,以点-线或线接触为主;胶结作用以不同类型黏土矿物为主,总体处于中成岩A12-A21微期有利阶段;研究区经历了酸性和碱性溶蚀作用,以典型高岭石和绿泥石酸-碱性溶蚀作用产物最为突出;分流河道A11微期高岭石和分流河道A12微期高岭石沉积-成岩相是研究区优质储层发育相带。

       

      Abstract: In order to explore the diagenesis and development pattern of high-quality reservoirs of the Weizhou Formation in the Weixinan Depression of Beibu Gulf Basin, South China Sea, taking the third section of the Weizhou Formation in the Weizhou X Oilfield as an example, the types and mechanisms of diagenesis, the sequence of diagenesis evolution, and the division of diagenetic facies were analyzed in depth through techniques such as thin section microscopy identification, scanning electron microscopy, cathodoluminescence, and numerical simulation of diagenesis. The main controlling factors and selection of high-quality reservoirs were also carried out. The results show that the compaction effect of the reservoir in the third section of the study area is moderate, mainly in point line or line contact; The cementation process is mainly composed of different types of clay minerals, and is generally in the favorable stage of A12-A21 micro stage of diagenesis; The research area has experienced acidic and alkaline dissolution, with typical kaolinite and chlorite acid alkaline dissolution products being the most prominent; The sedimentary diagenetic facies of distributary channel A11 and distributary channel A12 are the development facies zones of high-quality reservoirs in the study area.

       

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