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    大庆徐家围子凹陷登娄库组三段层序地层旋回分析

    赵国连

    赵国连. 大庆徐家围子凹陷登娄库组三段层序地层旋回分析[J]. 沉积与特提斯地质, 1999, 19(4): 35-41.
    引用本文: 赵国连. 大庆徐家围子凹陷登娄库组三段层序地层旋回分析[J]. 沉积与特提斯地质, 1999, 19(4): 35-41.
    ZHAO Guo-lian. Sequence stratigraphic cycles of the third member of the Denglouku Formation in the Xujiaweizi subsidence, Daqing, northeastern China[J]. Sedimentary Geology and Tethyan Geology, 1999, 19(4): 35-41.
    Citation: ZHAO Guo-lian. Sequence stratigraphic cycles of the third member of the Denglouku Formation in the Xujiaweizi subsidence, Daqing, northeastern China[J]. Sedimentary Geology and Tethyan Geology, 1999, 19(4): 35-41.

    大庆徐家围子凹陷登娄库组三段层序地层旋回分析

    基金项目: 

    国家自然科学基金委员会与大庆石油管理局联合资助项目(49894190)

    详细信息
    • 中图分类号: P534.53

    Sequence stratigraphic cycles of the third member of the Denglouku Formation in the Xujiaweizi subsidence, Daqing, northeastern China

    • 摘要: 本文从沉积相、岩性和测井相入手,分析了下白垩统登娄库组三段岩性发育及相类型,并划分了层序旋回,识别出各旋回体系域归属。并对上述划分用Fischer点图进行检验,证明上述分析是合理的。同时,本文指出,Fischer点图在旋回识别上有独到之处。
      Abstract: The third member of the Denglouku Formation is a prospect area for the oil and gas resources in the Xujiaweizi subsidence, Daqing, northeastern China. In this paper, the lithology and sedimentary facies are discussed, and sequence stratigraphic cycles and their systems tracts am discriminated on the basis of sedimentary facies, lithology and well logs. The classification has been verified by using Fischer's plots, which may be a potential tool for sequence analysis.
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    出版历程
    • 收稿日期:  1999-02-07
    • 修回日期:  1999-05-18
    • 发布日期:  1999-08-29

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