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白家海凸起—阜北斜坡八道湾组储层特征研究
引用本文:况昊,瞿建华,王振奇,柳妮,马文睿.白家海凸起—阜北斜坡八道湾组储层特征研究[J].西南石油大学学报(社会科学版),2014,34(2):29-36.
作者姓名:况昊  瞿建华  王振奇  柳妮  马文睿
作者单位:1.“油气资源与勘探技术”教育部重点实验室(长江大学),湖北荆州4340232. 长江大学地球科学学院,湖北荆州4340233. 中国石油新疆油田分公司勘探开发研究院,新疆克拉玛依8340004. 同济大学海洋与地球科学学院,上海虹口200092
摘    要:利用岩石薄片、铸体薄片鉴定、X–衍射、扫描电镜和压汞等资料,对白家海凸起—阜北斜坡侏罗系八道湾组的储层特征进行了研究,分析了储层的成岩作用类型、成岩演化序列、成岩作用对孔隙结构的影响及孔隙演化史。研究结果表明:八道湾组储层以岩屑砂岩为主储集空间以粒内溶孔和粒间溶孔为主,孔隙度经历了多期的演化过程,由原始的高孔隙度演化为现今低孔隙度。

关 键 词:白家海凸起    阜北斜坡    八道湾组    储层特征

Study on Reservoir Characteristics in Badaowan Formation,BaijiahaiUplift—Fubei Slope
Kuang Hao,Qu jianhua,Wang Zhenqi,Liu Ni,Ma Wenrui.Study on Reservoir Characteristics in Badaowan Formation,BaijiahaiUplift—Fubei Slope[J].Journal of Southwest Petroleum University(Social Sciences Edition),2014,34(2):29-36.
Authors:Kuang Hao  Qu jianhua  Wang Zhenqi  Liu Ni  Ma Wenrui
Institution:1. MOE Key Laboratory of Exploration Technologies of Oil and Gas Resources,Yangtze University,Jingzhou,Hubei 434023,China2. College of Geoscience,Yangtze University,Jingzhou,Hubei 434023,China3. Xinjiang Oilfield Company,PetroChina,Karamay,Xinjiang 834000,China4. School of Ocean and Earth Science,Tongji University,Hongkou,Shanghai 200092,China
Abstract:By observing thin-sections and casting thin-sections,and analysing materials X-ray diffraction,scanning electronmicroscope(SEM)and mercury injection and so on,we carry out a comprehensive research on the features of Jurassic petrologyand pore structure in Baijiahai Uplift—Fubei Slope. Types of diagenesis and diagenetic evolution sequences,the impact ofdiagenesis on pore structure and pore evolution are also studied for this research. Crossplots of electric well logs and acousticimpedance are applied to identify different lithologic characters. The results are that the lithology in the studies area is mainlylithic sandstone;the crossplots can well distinguish lithologies in the field,and that the reservoir in the field is evolved fromoriginal high-porosity to low-porosity type nowadays.
Keywords:Baijiahai Uplift                                                                                                                        Fubei Slope                                                                                                                        Badaowan Formation                                                                                                                        physical property
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