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ZHANG Xi-lin, ZHU Xiao-min, ZHONG Da-kang, LIANG Bing, CAO Bing, HE Xiang-yang. The Character of Sequence Framework of Tertiary and Upper Cretaceous in Gaoyou Sag, Subei Basin[J]. Acta Sedimentologica Sinica, 2004, 22(3): 393-399.
Citation: ZHANG Xi-lin, ZHU Xiao-min, ZHONG Da-kang, LIANG Bing, CAO Bing, HE Xiang-yang. The Character of Sequence Framework of Tertiary and Upper Cretaceous in Gaoyou Sag, Subei Basin[J]. Acta Sedimentologica Sinica, 2004, 22(3): 393-399.

The Character of Sequence Framework of Tertiary and Upper Cretaceous in Gaoyou Sag, Subei Basin

  • Received Date: 2003-06-10
  • Rev Recd Date: 2004-03-10
  • Publish Date: 2004-09-10
  • Based on the analysis of seismic data, borehole and well-logging,core and paleontology of Tertiary and upper Cretaceous with thickness of more than 7000m in Gaoyou Sag, Subei Basin, two first-level sequences, four second-level sequences and 11 third-sequences have been identified. System tracts were also identified within each sequence based on the maximum flooding surface and fault-break(first flooding surface). Each of the 11 sequences consists of either complete lowstand, transgressive and highstand system tracts or one or two of them. Due to the different activity of Hanliu fault in the east and west part of Gaoyou sag, the west part is characterized by bi-fault subsiding basin, and the east part single-fault basin. Based on structural analysis, sequence pattern in Gaoyou sag may be described as the west part with fault-break and east without break. The main controlling factors of sequence stratigraphy was analyzed and were believed to be tectonics and climate.
  • [1] 朱筱敏.层序地层学.山东东营:石油大学出版社,2000. 1~207[Zhu Xiaomin. Sequence Stratigraphy. Dongying Shandong: Press of University of Petroleum, 2000. 1~207]
    [2] 赵澄林,朱筱敏.沉积岩石学.北京:石油工业出版社,2000.33~89[Zhao Chenglin, Zhu Xiaomin. Sedimentary lithology. Beijing: Petroleum Industry Press, 2000. 33~89]
    [3] 顾家裕.陆相层序地层学格架概念及模式.石油勘探与开发,1995,22(4):6~10[Gu Jiayu. Framework concepts and models of sequence stratigraphy in nonmarine petroliferous basin.Petroleum Exploration & Development, 1995, 22(4): 6~10]
    [4] 顾家裕,张兴阳. 油气沉积学发展回顾和应用现状.沉积学报,2003,21(1):137~141[Gu Jiayu, Zhang Xingyang. Development review and current application of petroleum sedimentology. Acta Sedimentologica Sinica, 2003,21(1): 137~141
    [5] 朱筱敏,康安,王贵文.陆相坳陷型和断陷型湖盆层序地层样式探讨.沉积学报,2003,21(2):283~287[Zhu Xiaomin, Kang An, Wang Guiwen. Sequence stratigraphic models of depression and faulted-down lake basins. Acta Sedimentologica Sinica, 2003,21(2): 283~287]
    [6] 许淑梅,翟世奎,李三忠,等.歧口凹陷滩海区下第三系层序地层分析及沉积体系研究.沉积学报, 2001,19(3): 362~367[Xu Shumei, Zhai Shikui, Li Sanzhong, et al. Ananalysis on sequence stratigraphy and sedimentary system of early Neocene in Qikou sag. Acta Sedimentologica Sinica, 2001, 19(3): 362~367]
    [7] 胡宗全,朱筱敏.具有地形坡折带的坳陷湖盆层序地层模拟.沉积学报, 2002,20(2): 217~221[Hu Zongquan, Zhu Xiaomin.Sequence stratigraphic simulation of depression lake basin with topographic ramp. Acta Sedimentologica Sinica, 2002, 20(2): 217~221]
    [8] 张善文,王英民,李群.应用坡折带理论寻找隐蔽油气藏.石油勘探与开发,2003,30(3):5~7[Zhang Shanwen,Wang Yingmin, Li Qun. Searching subtle traps using the theory of slope break . Petroleum Exploration & Development, 2003, 30(3): 5~7]
    [9] 孙龙德.东营凹陷北部斜坡带沙三-四段砂砾岩体与油气聚集.沉积学报, 2003,21(2):278~282[Sun Longde, Sandstone-conglomerate bodies in Sha3-4 Members and hydrocarbon accumulation in northern slope of Dongying Sag. Acta Sedimentologica Sinica, 2003,21(2): 278~282]
    [10] Van Wagoner J C, Motchum R M, et al. Siliciclastic sequence stratigraphy in well logs, cores, and outcrops: concepts for high resolution correlation of time and facies. AAPG Methods in Exploration Series, 1990, 55:1~240
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  • Received:  2003-06-10
  • Revised:  2004-03-10
  • Published:  2004-09-10

The Character of Sequence Framework of Tertiary and Upper Cretaceous in Gaoyou Sag, Subei Basin

Abstract: Based on the analysis of seismic data, borehole and well-logging,core and paleontology of Tertiary and upper Cretaceous with thickness of more than 7000m in Gaoyou Sag, Subei Basin, two first-level sequences, four second-level sequences and 11 third-sequences have been identified. System tracts were also identified within each sequence based on the maximum flooding surface and fault-break(first flooding surface). Each of the 11 sequences consists of either complete lowstand, transgressive and highstand system tracts or one or two of them. Due to the different activity of Hanliu fault in the east and west part of Gaoyou sag, the west part is characterized by bi-fault subsiding basin, and the east part single-fault basin. Based on structural analysis, sequence pattern in Gaoyou sag may be described as the west part with fault-break and east without break. The main controlling factors of sequence stratigraphy was analyzed and were believed to be tectonics and climate.

ZHANG Xi-lin, ZHU Xiao-min, ZHONG Da-kang, LIANG Bing, CAO Bing, HE Xiang-yang. The Character of Sequence Framework of Tertiary and Upper Cretaceous in Gaoyou Sag, Subei Basin[J]. Acta Sedimentologica Sinica, 2004, 22(3): 393-399.
Citation: ZHANG Xi-lin, ZHU Xiao-min, ZHONG Da-kang, LIANG Bing, CAO Bing, HE Xiang-yang. The Character of Sequence Framework of Tertiary and Upper Cretaceous in Gaoyou Sag, Subei Basin[J]. Acta Sedimentologica Sinica, 2004, 22(3): 393-399.
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