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Article Navigation >  Acta Sedimentologica Sinica  > 2005  >  23(3): 498-506

WANG Ying, WANG Ying-min, WANG Xiao-zhou, XIN Ren-chen, ZHAO Zhi-kui, ZHAO Zhan-yin. The Origin and Evolution of Slope Break Belt and Its Effect on Stratigraphy Distr ibution in Large Down-warped Lake Basin[J]. Acta Sedimentologica Sinica, 2005, 23(3): 498-506.
Citation: WANG Ying, WANG Ying-min, WANG Xiao-zhou, XIN Ren-chen, ZHAO Zhi-kui, ZHAO Zhan-yin. The Origin and Evolution of Slope Break Belt and Its Effect on Stratigraphy Distr ibution in Large Down-warped Lake Basin[J]. Acta Sedimentologica Sinica, 2005, 23(3): 498-506.
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The Origin and Evolution of Slope Break Belt and Its Effect on Stratigraphy Distr ibution in Large Down-warped Lake Basin

  • 1.

    Exploration Institute of CNOOC Research Certer, Gaobeidian Hebei 074010;

  • 2.

    Key Laboratory for Hydrocarbon Accumulation, Ministry of Education, Beijing 102249;

  • 3.

    The Basin and Reservoir Research Center, University of Petroleum, Beijing 102249;

  • 4.

    Institute of Marine Geology and Geophysics, China University of Geoscience, Beijing 100083;

  • 5.

    The Jilin Oil-field Corporation, CNPC, Songyuan Jilin 138001

  • Received Date: 2004-10-14
  • Rev Recd Date: 2004-12-21
  • Publish Date: 2005-09-10
  • The slope belt developped in large-type down-warped lake basin is similar to the slope in the marine basin.The Songliao Basin can be identified as two slope belts, and this paper analyzes the origin and evolution of slope belt and its effect on sediment system and stratigraphy distribution. The two slope belts are all influenced by the fault during the early periods. With the development of slope belt Taobao-Shuangang high water level slope is controlled by the direction of provenance and erosion, but the sediment supply and the differential compaction are main controlling factors in the development of Honggang-Haituozi low water level slope. The evolvement of the sediment system is controlled by the Taobao-Shuangang high water level slope and groove, but the Honggang-Haituozi low water level slope controls the range of lower system tract.
  • [1] 1 Stow D A V,Mayall M. Deep-Water sedimentary systems:New models for the 21st century[J]. Marine and Petroleum Geology,2000.125-135.

    2 王英民,刘豪,李立诚. 准噶尔大型坳陷湖盆坡折带的类型和分布特征[J].地球科学-中国地质大学学报,2002,(06):683-688.

    3 赵玉光,丘东洲. 准噶尔界山前陆盆地晚期(T-J)层序地层与油气勘探[J].新疆石油地质,1993,(04):323-331.

    4 魏魁生,叶淑芬,郭占谦. 松辽盆地白垩系非海相沉积层序模式[J].沉积学报,1996,(04):50-60.

    5 樊太亮,李卫东. 层序地层学应用于陆相油藏预测的成功实例[J].石油学报,1999,(02):12-17.

    6 林畅松,潘元林,肖建新. "构造坡折带"-断陷盆地层序分析和油气预测的重要概念[J].地球科学-中国地质大学学报,2000,(03):260-266.

    7 王英民,金武弟,刘书会. 断陷湖盆多级坡折带的成因类型、展布及其勘探意义[J].石油与天然气地质,2003,(03):199-203.

    8 刘豪,王英民,王媛. 大型坳陷湖盆坡折带的研究及其意义-以准噶尔盆地西北缘侏罗纪坳陷湖盆为例[J].沉积学报,2004,(01):95-102.

    9 刘豪,王英民,王媛. 坳陷湖盆坡折带特征及其对非构造圈闭的控制[J].石油学报,2004, (01):30-35.

    10 刘豪,王英民. 准噶尔盆地坳陷湖盆坡折带在非构造圈闭勘探中的应用[J].石油与天然气地质,2004,(04):422-427.

    11 Vail P R,Mitchum R M,Todd R G. Seismic stratigraphy and global changes of sea level[A].AAPG,1977.49-212.

    12 张善文,王英民,李群. 应用坡折带理论寻找隐蔽油气藏[J].石油勘探与开发,2003,(03):5-7.

    13 辛仁臣,蔡希源,王英民. 松辽坳陷深水湖盆层序界面特征及低位域沉积模式[J].沉积学报,2004,(03):387-392.

    14 王永春. 松辽盆地南部岩性油藏的形成和分布[M].北京:石油工业出版社,2001.26-31.
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  • Received:  2004-10-14
  • Revised:  2004-12-21
  • Published:  2005-09-10

The Origin and Evolution of Slope Break Belt and Its Effect on Stratigraphy Distr ibution in Large Down-warped Lake Basin

  • 1. Exploration Institute of CNOOC Research Certer, Gaobeidian Hebei 074010;
  • 2. Key Laboratory for Hydrocarbon Accumulation, Ministry of Education, Beijing 102249;
  • 3. The Basin and Reservoir Research Center, University of Petroleum, Beijing 102249;
  • 4. Institute of Marine Geology and Geophysics, China University of Geoscience, Beijing 100083;
  • 5. The Jilin Oil-field Corporation, CNPC, Songyuan Jilin 138001
  • Received Date: 2004-10-14
  • Rev Recd Date: 2004-12-21
  • Publish Date: 2005-09-10

Abstract: The slope belt developped in large-type down-warped lake basin is similar to the slope in the marine basin.The Songliao Basin can be identified as two slope belts, and this paper analyzes the origin and evolution of slope belt and its effect on sediment system and stratigraphy distribution. The two slope belts are all influenced by the fault during the early periods. With the development of slope belt Taobao-Shuangang high water level slope is controlled by the direction of provenance and erosion, but the sediment supply and the differential compaction are main controlling factors in the development of Honggang-Haituozi low water level slope. The evolvement of the sediment system is controlled by the Taobao-Shuangang high water level slope and groove, but the Honggang-Haituozi low water level slope controls the range of lower system tract.

WANG Ying, WANG Ying-min, WANG Xiao-zhou, XIN Ren-chen, ZHAO Zhi-kui, ZHAO Zhan-yin. The Origin and Evolution of Slope Break Belt and Its Effect on Stratigraphy Distr ibution in Large Down-warped Lake Basin[J]. Acta Sedimentologica Sinica, 2005, 23(3): 498-506.
Citation: WANG Ying, WANG Ying-min, WANG Xiao-zhou, XIN Ren-chen, ZHAO Zhi-kui, ZHAO Zhan-yin. The Origin and Evolution of Slope Break Belt and Its Effect on Stratigraphy Distr ibution in Large Down-warped Lake Basin[J]. Acta Sedimentologica Sinica, 2005, 23(3): 498-506.
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