WU Shi-guo, SUN Yong-zhuang, SONG Jian-yong. ANALYSIS OF SEQUENCE STRATIGRAPHY OF THE 3RD MEMBER OF SHAHEJIE FORMATION IN THE BOXING SUB-DEPRESSION,JIYANG DEPRESSION[J]. Marine Geology & Quaternary Geology, 2006, 26(3): 101-107.
Citation: WU Shi-guo, SUN Yong-zhuang, SONG Jian-yong. ANALYSIS OF SEQUENCE STRATIGRAPHY OF THE 3RD MEMBER OF SHAHEJIE FORMATION IN THE BOXING SUB-DEPRESSION,JIYANG DEPRESSION[J]. Marine Geology & Quaternary Geology, 2006, 26(3): 101-107.

ANALYSIS OF SEQUENCE STRATIGRAPHY OF THE 3RD MEMBER OF SHAHEJIE FORMATION IN THE BOXING SUB-DEPRESSION,JIYANG DEPRESSION

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  • Received Date: November 07, 2005
  • Revised Date: December 27, 2005
  • The authors carried out the analysis of sequence stratigraphy of the 3rd member of Shahejie Formation in western Boxing sub-depression with high-resolution sequence stratigraphy with base level as the reference surface.Five sequence boundaries and four flooding surfaces are recognized in the 3rd member of Shahejie Formation. According to these surfaces,the member is divided into four long-term base level cycles. Moreover,there are eight medium-scale base level cycles through recognizing inner turnaround surfaces of the long-term base level cycles. High-resolution sequence stratigraphic framework is constructed through correlations among wells and seismic profiles. Characters and depositional evolutions of each sequence are analyzed in the sequence framework. Based on the above analysis,sequence stratigraphic models for braided river delta to turbidite fan are constructed.Braided river deltas and turbidite fans have the upgrading characters; the former are distributed in slope areas and the latter are generally distributed in depression areas.Braided river deltas are concentrated in the falling hemi-cycles of base level and turbidite fans in the rising hemi-cycles.The scales of turbidite fans are relative to lake flooding surfaces. We draw a conclusion that turbidite fan is the main type of reservoir to lithologic traps.The favorite members to lithologic traps are the rising hemi-cycles of MSC5,MSC6,MSC7 and MSC8;and the favorite areas to lithologic traps are the depressions at the break of the south slope of Boxing sub-depression.
  • [1]
    徐怀大.层序地层学理论用于我国断陷盆地分析中的几个问题[J].石油与天然气地质1997,18(1):83-89.

    [XU Huai-da,Some problems existed in the theory of sequence stratigraphy applied in the fault basin of China[J]. Oil and Gas Geology,1997,18(1):83-89.]
    [2]
    徐怀大,译,层序地层学原理(海平面变化综合分析)[M].北京:石油工业出版社,1993.[XU Huai-da (translation).Sequence Straitgraphy[M]. Beijing:Petroleum Industry Press,1993.]
    [3]
    邓宏文,王红亮,祝永军.美国层序地层研究中的新学派——高分辨率层序地层学[J].石油与天然气地质,1995,16(2):89-97.

    [DENG Hong-wen,WANG Hong-liang,ZHU Yong-jun.Tim cross,theory and application of sequence stratigraphic base-levels and their application[J].Oil and Gas Geology,1995,16(2):89-97.]
    [4]
    邓宏文,王红亮,祝永军.高分辨率层序地层学——原理及应用[M].北京:地质出版社,2002.[DENG Hong-wen,WANG Hong-liang,ZHU Yong-jun.Theory and Application of high-resolution Seismic Stratigraphy[M].Beijing:Geological Publishing House,2002.]
    [5]
    Cross T A.High-resolution stratigraphic correlation from the perspectives of base-level cycles and sediment accommodation[C]//In:Dolson J M (ed). Unconformity related hydrocarbon exploration and accumulation in clastic and carbonate settings.Short Course Notes,Rocky Mountain Association of Geologists,1991:28-42.
    [6]
    Cross T A,Lessenger M A.Construction and application of a stratigraphic inverse model[C]//In:Harbaugh J W,Watney W L,Rankey E C,et al(eds).Numerical Experiments in Stratigraphy:Recent Advances in Stratigraphic and Sedimentologic Computer Simulation. SEPM Special publication 62,1999:69-83.
    [7]
    邓宏文,王洪亮,李熙哲.层序地层地层基准面的识别、对比技术及应用[J].石油与天然气地质,1996,17(3):177-184.

    [DENG Hong-wen,WANG Hong-liang,LI Xi-zhe.Identification and correlation techniques of sequence stratigraphic base-levels and their application[J]. Oil and Gas Geology,1996,17(3):177-184.]
    [8]
    冯有良.东营凹陷下第三系层序地层格架及盆地充填样式[J].地球科学,1999,24(6):635-642.

    [FENG You-liang.Lower Tertiary sequence stratigraphic framework and basin filling model in the Dongying depression[J].Earth Sciences,1999,24(6):635-642.]
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