北部湾盆地海中凹陷涠三段滩坝砂体沉积发育特征及主控因素

    Sedimentary development characteristics and main controlling factors of beach-bar sand bodies in Haizhong depression, Beibuwan basin

    • 摘要: 北部湾盆地海中凹陷多口钻井已获得高产油气流突破,证实了其具有良好的勘探潜力,因此对其沉积发育特征及主控因素的研究具有重要意义。从岩芯相出发,结合研究区测井相分析滩坝砂体特征,并以地震相为基础,结合属性、古地貌确定沉积相类型,在此基础上建立涠三段滩坝砂体沉积模式,并探讨其主控因素。研究结果表明,岩芯相上,滩坝砂体往往发育砂纹交错层理、平行层理和风暴沉积序列,概率粒度累积曲线上呈“四段式”特征;测井相上表现为连续多个反旋回漏斗形测井相特征;地震相上呈现微丘状反射和强振幅波状地震反射特征;平面上滩坝砂体发育在涠西南低凸起西南倾末端及南部缓坡带西侧;纵向上滩坝砂体互相叠置,体现了体现了滩坝砂体随湖平面升降频繁迁移、多期叠置的沉积特点。古地貌、古物源和古水深及湖平面变化控制了滩坝砂体的位置和展布范围,其中古地貌通过沟-槽-渠、低凸-鼻凸-古梁控制了滩坝砂体的发育位置,滩坝砂体发育在古地貌水下隆起区和缓坡凸起区;古物源决定了相关滩坝砂体发育规模;古水深及周缘河流、湖浪、沿岸湖流方向通过决定滨-浅-深湖范围,进而控制滩坝砂体的展布范围。本文研究结果可为相似地质条件的滩坝储层未来油气勘探提供的一定的参考价值。

       

      Abstract: Numerous wells within the Haizhong depression of the Beibuwan basin have demonstrated significant advancements in oil and gas extraction, indicating promising exploration prospects. Consequently, investigating the sedimentary evolution patterns and influential factors in this region is crucial. By examining core and well logging facies, this study analyzes the attributes of beach bar sand bodies and identifies sedimentary facies through seismic facies analysis, attribute assessment, and paleogeomorphological considerations. The findings indicate that beach bar sand bodies exhibit distinct characteristics across different facies: (1) Within core facies, these sand bodies commonly display features such as sand cross-bedding, parallel bedding, storm sedimentary sequences, and a "four-stage" pattern in probability grain size accumulation curves. In logging facies, they demonstrate continuous funnel-type logging facies with multiple reverse cycles, while seismic facies show micro-hump reflections and strong amplitude wave seismic reflections. Geographically, beach bar sand bodies tend to develop at the southwest dip end of the Weisouthwest low uplift and the western side of the southern gentle slope belt,the longitudinal upper beach bar sand bodies exhibit mutual superposition, indicating the sedimentary features of frequent migration and multi-stage superposition of beach bar sand bodies in response to fluctuations in lake levels.. (2) The positioning and distribution of beach bar sand bodies are influenced by factors such as paleogeomorphology, ancient sources, paleo-water depth, and fluctuations in lake levels. Specifically, paleogeomorphology dictates the development position of these sand bodies through trench-channel formations, low-convex-nose-convex-ancient ridges, and their occurrence in underwater uplift and gentle slope uplift areas. Ancient sources determine the scale of development of beach bar sand bodies. Additionally, paleo-depth, as well as the direction of surrounding rivers, lake waves, and coastal lake flow, influence the range from shore to shallow to deep lake, thereby controlling the distribution of beach bar sand bodies. The findings of this study offer insights that may prove valuable for future exploration of oil and gas reserves in beach bar reservoirs with similar geological settings.

       

    /

    返回文章
    返回