摘要
车西洼陷沙四上亚段碎屑岩储层以含泥细砂岩为主,孔隙度多集中在10%～20%,渗透率多小于10×10-3μm2,结合铸体薄片、压汞、地化测试分析等综合评价为中-低孔特低渗较差储层。研究表明,该区储层物性主要受沉积、成岩和异常高压3种因素控制:1)沉积微相主控储层砂体空间展布形态及孔隙度分布特征;2)成岩作用主控储层砂体孔喉结构演化及渗透率分布特征;3)异常高压对孔隙度和渗透率的影响则相对均衡,且与二者异常高值深度带相对应。上述主控因素对特低渗储层孔隙度和渗透率影响程度的差异性,以及高压发育不同阶段对储层孔隙结构组合特征的影响等仍需要进一步深入研究,势必对同类型油气藏的勘探与开发产生深远影响。
Detrital rock reservoir of upper Es4 member in Chexi Depression is mainly shaly fine sandstone,with porosity being 10%-20% mostly and with permeability less than 10 md.Combined with the analysis of casting thin section,mercury injection and geochemistry test,the reservoir is evaluated as middle-low porosity and ultra-low permeability reservoir.The study shows that the reservoir property is mainly controlled by sedimentary microfacies,diagenesis and abnormal overpressure.The spatial distribution and porosity distribution of reservoir sandstones are mainly controlled by sedimentary microfacies.Disgenesis dominates the pore throat structure evolution and permeability distribution of sand body.Abnormal overpressure has an equal effect on porosity and permeability and is corresponding with the depth zone of abnormal high value of both.The differences of three controlling factors to the effect degree of porosity and permeability of ultra-low permeability reservoirs and the effect of the overpressure in different reservoir development stages on the combination characteristics of pore structure require to be studied further,which will create the great effect for the exploration and development of similar reservoirs.
出处
《断块油气田》
CAS
北大核心
2011年第4期424-428,共5页
Fault-Block Oil & Gas Field
基金
国家科技重大专项"大型油气田及煤层气开发"项目(2008ZX05004)
中国石油科技创新基金"泥岩非构造裂缝形成机理
分布规律及其对油气成藏的影响"项目(2010D-5006-0104)
关键词
特低渗储层
物性
沉积微相
成岩作用
异常高压
ultra-low permeability reservoir
physical property
sedimentary microfacies
diagenesis
abnormal overpressure
