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作 者:郭岭[1,2] 孙遥 郭峰 张翠萍 GUO Ling;SUN Yao;GUO Feng;ZHANG Cuiping(State Key Laboratory of Continental Dynamics,Northwest University,Xi’an 710069,Shaanxi,China;Department of Geology,Northwest Uni-versity,Xi’an 710069,Shaanxi,China;School of Earth Science and Engineering,Xi’an Shiyou University,Xi’an 710065,Shaanxi,China;The Sixth Oil Production Factory,Changqing Oilfield Company,Xi’an 710016,Shaanxi,China)
机构地区:[1]西北大学大陆动力学国家重点实验室,陕西西安710069 [2]西北大学地质学系,陕西西安710069 [3]西安石油大学地球科学与工程学院,陕西西安710065 [4]长庆油田公司第六采油厂,陕西西安710016
出 处:《河南理工大学学报(自然科学版)》2023年第4期76-85,共10页Journal of Henan Polytechnic University(Natural Science)
基 金:国家自然科学基金资助项目(41302076);陕西省自然科学基金资助项目(2014JQ5191)。
摘 要:采用粒度分析、真空浸渍铸体薄片分析、扫描电镜检测、压汞测试、黏土矿物X射线衍射和常规物性分析等方法探究胡尖山油田延长组长6段三角洲前缘致密砂岩储层特征及其主控因素。结果表明:长6段储层致密砂岩主要为岩屑长石砂岩和长石岩屑砂岩,岩石成分成熟度和结构成熟度均较低;主要孔喉组合为残余粒间孔+长石溶孔+晶间孔的小孔-微细喉道组合,孔隙度和渗透率均值分别为10.70%,0.69×10^(-3)μm^(2);孔渗相关性较好,为低孔特低孔-特低渗超低渗小孔微细喉道型储层,渗透率主要由数量较少的微孔、中孔贡献,孔隙度主要由数量较多的微米孔贡献;强烈的压实、泥质、碳酸盐胶结作用是长6段储层致密的主要原因;水下分流河道等优势沉积相带和溶蚀作用是储层形成的主控因素。The characteristics and main controlling factors of tight sandstone reservoirs of Chang 6 member,Yanchang Formation in Hujianshan Oilfield have been studied by particle size analysis,thin section,scan-ning electron microscopy detection,mercury intrusion testing,X-ray diffraction,and conventional physical property analysis.The results showed that the tight sandstone of Chang 6 member was mainly detritus feld-spar sandstone and feldspar detritus sandstone.The maturity of rock composition and structure was relatively low.The main pore throat assemblage included intergranular pore,feldspar dissolution pore and intercrystal-line pore.Average porosity and permeability were 10.70%and 0.69×10^(-3)μm^(2)respectively.The tight sand-stone of Chang 6 member in Hujianshan Oilfield was an ultra-low porosity,ultra-low permeability reservoir.There was a positive correlation between porosity and permeability.Permeability was mainly contributed by a small number of micropores and mesopores,while porosity was mainly contributed by a large number of mi-cron pores.The mechanism of reservoir densification included compaction and argillaceous,carbonate cemen-tation.The underwater distributary channel facies was the dominant sedimentary facies for the formation of high-quality reservoir.Dissolution was one of the main controlling factors for the formation of the reservoirs.
关 键 词:三角洲前缘 致密砂岩储层 胡尖山油田 长6段 鄂尔多斯盆地
分 类 号:TE122[石油与天然气工程—油气勘探]
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