安塞油田王窑地区长6油层沉积微相研究
Sedimentary microfacies of the Chang-6 reservoir of Yanchang Formation in Wangyao district, Ansai oilfield
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摘要: 王窑地区长6油层为湖泊河控三角洲前缘沉积,主要沉积微相为三角洲前缘水下分流河道、分流河口砂坝、前缘砂席和分流间等。水下分流河道充填沉积为向上变细的砂岩层序,分流河口砂坝可划分为向上变粗的前积式和非前积式两种沉积层序类型。水下分流河道和河口砂坝砂体相互连接,形成厚度较稳定的三角洲前缘复合体。该区三角洲沉积是安塞三角洲发育较晚的一支,也是指状砂体伸入湖区最远、发育程度最高的分支。长612沉积期,为三角洲的初始进积阶段,三角洲沉积由两支分流组成。长611沉积期三角洲前缘体系完整,砂体发育,分流带相互叠置交错。根据岩心描述结果、结合砂体形态和连井剖面对比分析,对长6油层三角洲沉积微相进行了综合表征,并提出了开发调整意见,为王窑地区特低渗透油田的高效开发奠定了地质基础。Abstract: The origins of Chang-6 reservoir horizons in Wangyao district of Ansai oilfield are interp reted to be a river-dom inated delta deposited in lacustrine environm ent.The main sedimentary microfacies of Chang-6 reservoir horizons in Wangyao district include distributary channel,distribu tary mouthbar,front sand sheet and in terdist ributary deposits.The distributary channel fills to show a finning upward sequence.The distributary mouthbar deposits consist of overall coarsing upward sequence and other homogeneous sequences.The distributary channel and distributary mouthbar sands coalesce to constitute the dominated petroleum reservoirs.Prog radation of two distributa ries constructed at first only a delta skeleton in the Chang-612 sand layer.Rapid sed imentation during the period of Chang-611 lead to rapid progradation basinward of multiple distributa ries.The deltaic microfacies are interpreted and delineated based on depositional sequence and sandbody geometry.Sandbody microfacies are the main factors affecting movement of oil and water.Comprehen sive descriptions of sedimentary microfacies are good methods to predict reservoir performance.
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