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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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    卫城油田卫81断块沙四段高分辨率层序地层学研究

    胡书毅, 文玲, 田海芹

    胡书毅, 文玲, 田海芹. 卫城油田卫81断块沙四段高分辨率层序地层学研究[J]. 西北地质, 2002, 35(2): 46-54.
    引用本文: 胡书毅, 文玲, 田海芹. 卫城油田卫81断块沙四段高分辨率层序地层学研究[J]. 西北地质, 2002, 35(2): 46-54.
    HU Shu-yi, WEN Ling, TIAN Hai-qin. Study of the high resolution sequence stratigraphy of Sha-4 member in Wei-81 fault block,Weicheng oil field[J]. Northwestern Geology, 2002, 35(2): 46-54.
    Citation: HU Shu-yi, WEN Ling, TIAN Hai-qin. Study of the high resolution sequence stratigraphy of Sha-4 member in Wei-81 fault block,Weicheng oil field[J]. Northwestern Geology, 2002, 35(2): 46-54.

    卫城油田卫81断块沙四段高分辨率层序地层学研究

    Study of the high resolution sequence stratigraphy of Sha-4 member in Wei-81 fault block,Weicheng oil field

    • 摘要: 通过钻井、测井、古生物等资料的综合分析,应用陆相层序地层学理论对卫城油田卫81断块沙四段进行高分辨率层序地层学研究.依据岩性、构造、古生物、测井等标志将沙四段划分出1个三级层序,2个体系域、4个准层序组和18个准层序.其中,沙四下段为低水位体系域,主要发育洪水-漫湖沉积体系;沙四上段为湖侵体系域,主要发育湖泊三角洲沉积体系.烃源岩为沙四上段的暗色泥岩,储集层为沙四上段的湖泊三角洲砂体和沙四下段的洪水流砂体.
      Abstract: Based on the systematical analysis of drilling, logging data and palaeontology, using continental facies sequence stratigraphy, the high resolution stratig raphic sequence of Sha-4 member in Wai-81 f ault block, Weicheng oil field, was studied. On the basis of the lithological characteristics, tectonic evolution, palaeontology and logging, the Sha-4 member was divided into: 1 three order sequence, 2 systemt racts, 4 parasequencesets, 18 parasequence. The lower Sha-4 member consists of lowstand system tract which mainly developed flood flow depositionract, and upper Sha-4 member consists of trangressive system tract which mainly developed delta deposition tract. The source rocks are the dark grey mudstone of the upper Sha-4 member, and the reservoir is lake delta facies from upper Sha-4 and f lood flow deposition tract from lower Sha-4 member.
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    • 期刊类型引用(1)

      1. 束青林,赵辉,姜在兴,赵国光. 渤海湾盆地惠民凹陷商河地区古近系沙四上亚段滩坝沉积特征. 现代地质. 2023(05): 1232-1242 . 百度学术

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    出版历程
    • 收稿日期:  2001-06-26
    • 修回日期:  2001-09-28
    • 发布日期:  2002-06-04

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