ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

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    刘学刚, 崔智林, 王娟. 安塞油田塞160井区长6油层组沉积微相研究[J]. 西北地质,2008,41(3): 86-91.
    引用本文: 刘学刚, 崔智林, 王娟. 安塞油田塞160井区长6油层组沉积微相研究[J]. 西北地质,2008,41(3): 86-91.
    LIU Xue-gang., CUI Zhi-lin, WANG Juan. Sedimentary Microfacies of the Chang-6 Reservoir in the Vicinity of Sai 160 Well[J]. Northwestern Geology,2008,41(3): 86-91.
    Citation: LIU Xue-gang., CUI Zhi-lin, WANG Juan. Sedimentary Microfacies of the Chang-6 Reservoir in the Vicinity of Sai 160 Well[J]. Northwestern Geology,2008,41(3): 86-91.

    安塞油田塞160井区长6油层组沉积微相研究

    Sedimentary Microfacies of the Chang-6 Reservoir in the Vicinity of Sai 160 Well

    • 摘要: 为了确定安塞油田塞160井区长6油层组沉积微相展布特征,通过岩心观察、描述和实验分析,对研究区长6油层的沉积微相类型进行细化,对各小层沉积微相的平面展布进行研究。塞160井区长6为湖泊河控三角洲前缘亚相沉积,主要沉积微相为三角洲前缘水下分流河道、分流河口坝、水下分流间湾和前缘席状砂。研究区长6三角洲沉积体系代表了较完整的自旋回过程,长63沉积期,研究区的主体被向湖区方向推进的三角洲前缘水下分流河道占据;长62期,研究区主体仍为水下分流河道沉积,但延伸较长63近;长612期维持与长62沉积模式;长611期三角洲前缘亚相发育完整,分流相带相互叠置。

       

      Abstract: In order to confirm the sedim entary microfacies of Chang-6 reservoir in the vicinity of Sai 160 well,core observing and describing,experiment data analyzing,and observation of the distribution of microfacies were performed.The main sedimentary microfaces are distributary channel,the point bar,the inter-distributaries and sands.The delta deposits system of chang-6 reservoir stands for the complete process of gyration of itself.

       

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