岩性油气藏 ›› 2020, Vol. 32 ›› Issue (5): 93101.doi: 10.12108/yxyqc.20200510
黄杰1, 杜玉洪1, 王红梅1, 郭佳1, 单晓琨1, 苗雪1, 钟新宇2, 朱玉双2
UANG Jie1, DU Yuhong1, WANG Hongmei1, GUO Jia1, SHAN Xiaokun1, MIAO Xue1, ZHONG Xinyu2, ZHU Yushuang2
摘要: 为了明确二连盆地阿尔凹陷腾格尔组腾一下段储层微观孔隙结构和可动流体赋存特征,开展了扫描电镜、铸体薄片、X射线衍射、高压压汞、恒速压汞和核磁共振等实验研究。结果表明:①腾一下段储层微观孔隙结构分为3种类型,不同孔隙结构具有不同的可动流体赋存特征。②Ⅰ类大孔喉结构,孔喉组合主要为粒间孔-孔隙缩小型喉道和粒间孔-缩颈型喉道,喉道半径大,孔喉半径比小,核磁共振T2谱主要为左低右高双峰型,可动流体饱和度高;Ⅱ类孔隙结构,主要为粒间孔-片状喉道组合与溶蚀孔-片状喉道组合,T2谱主要为左高右低双峰型,可动流体饱和度中等;Ⅲ类孔隙结构,主要为粒间孔-片状喉道组合、溶蚀孔-片状喉道组合和晶间孔-管束状喉道组合,喉道半径小,T2谱为左单峰型,可动流体饱和度低。③储层物性、微观孔隙结构、黏土矿物含量对可动流体赋存具有重要影响,其中喉道特征是影响可动流体赋存的最主要因素,喉道半径越大,大喉道越多,可动流体饱和度越高。该研究成果对阿尔凹陷腾一下段储层的高效开发具有指导意义。
中图分类号:
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