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XU Shu tang, MA Wei min, WANG De ren, JIN Guang xing, LI Ji dong, YANG Yu e. Sequence Strata of Lower Cretaceous in Baiyinchagan Depression, Erlian Basin[J]. Acta Sedimentologica Sinica, 2004, 22(4): 644-650.
Citation: XU Shu tang, MA Wei min, WANG De ren, JIN Guang xing, LI Ji dong, YANG Yu e. Sequence Strata of Lower Cretaceous in Baiyinchagan Depression, Erlian Basin[J]. Acta Sedimentologica Sinica, 2004, 22(4): 644-650.

Sequence Strata of Lower Cretaceous in Baiyinchagan Depression, Erlian Basin

  • Received Date: 2003-10-04
  • Rev Recd Date: 2004-02-24
  • Publish Date: 2004-12-10
  • Based on drilling, logging and seismic data, classification correlation of sequence strata has been performed. Formation of lower Cretaceous can be divided into 3 super sequences and 6 tertiary sequences. Lithology, sedimentary facies, system development and formation stacking have also been studied. After these study we could clearly understand the background of sequence formation, deposition evolution, development of source reservoir seal and their association. It is believed that the evolution of Baiyinchagan depression began at its early stage with inherited development and reached its peak at late stage. The depression lasted three flooding, forming three sets of source rocks, which developed 4 types of sandbody with 3 sets of reservoir seal assemblage.
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    [2] 王立志,王德仁,王留忠.白音查干凹陷白垩系生、储、盖特征与油气聚集.断块油气田,1995,2(增刊):29~34[Wang Lizhi, Wang Deren, Wang Liuzhong. Source-Reservoir-Cap Characteristics and Its Hydrocarbon Accumulation of Cretaceous in Baiyinchagan Depression, Fault-Block Oil and Gas Field, 1995, 2(Suppl.): 29~34
    [3] 蒋飞虎,刘晓丽,杨静.白音查干凹陷早白垩世介形虫类组合特征与沉积环境.石油勘探与开发,1996,23(2):34~42[Jiang Feihu,Liu Xiaoli,Yang Jing. Ostracode assemblage and sedimentary environment of Early Cretaceous of Baiyinchagan Depression. Petroleum Exploration and Development, 1996,23(2): 34~42]
    [4] 威尔格斯 C K, 等著.徐怀大等译.层序地层学原理--海平面变化综合分析.北京:石油工业出版社,1993[Welgs C K, et al, eds. Xu Huaida translated. Sea-Level Changes: An Integrated Approach. Beijing: Petroleum Industry Press,1993 ]
    [5] 纪友亮,张世奇, 等.层序地层学原理及层序成因机制模式.北京:地质出版社,1998[Ji Youliang, Zhang Shiqi, et al. Sequence Stratigraphy Theory and Sequence Forming Mode. Beijing: Geological Publishing House, 1998]
    [6] 邓宏文,王宏量,祝永军, 等.高分辨率层序地层学--原理及应用.北京:地质出版社,2002[Deng Hongwen, Wang Hongliang, Zu Yongjun, et al. Theory and Application of High Resolution Sequence Stratigraphy. Beijing: Geological Publishing House,2002]
    [7] 张福顺,樊太亮,刘燕学,等.白音查干凹陷特殊岩性段在层序地层研究中的意义.江汉石油学院学报,2003,25(1):8~10[Zhang Fushun, Fan Tailiang, Zhu Yongjun, et al. Journal of Jianghan Petroleum Institute, 2003,25(1):8~10]
    [8] 中国石油天然气总公司勘探局编.层序地层学原理及应用.北京:石油工业出版社,1998[Exploration Bureau of CNPC. Theory and Application of Sequence Stratigraphy. Beijing: Petroleum Industry Press,1998]
    [9] 徐强,姜烨,董伟良, 等.中国层序地层研究现状和发展方向.沉积学报,2003,21(1):155~166[Xu Qiang, Jiang Ye, Dong Weiliang, et al. Research status and development direction of sequence stratigraphy in China. Acta Sedimentologica Sinica, 2003,21(1):155~166]
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  • Received:  2003-10-04
  • Revised:  2004-02-24
  • Published:  2004-12-10

Sequence Strata of Lower Cretaceous in Baiyinchagan Depression, Erlian Basin

Abstract: Based on drilling, logging and seismic data, classification correlation of sequence strata has been performed. Formation of lower Cretaceous can be divided into 3 super sequences and 6 tertiary sequences. Lithology, sedimentary facies, system development and formation stacking have also been studied. After these study we could clearly understand the background of sequence formation, deposition evolution, development of source reservoir seal and their association. It is believed that the evolution of Baiyinchagan depression began at its early stage with inherited development and reached its peak at late stage. The depression lasted three flooding, forming three sets of source rocks, which developed 4 types of sandbody with 3 sets of reservoir seal assemblage.

XU Shu tang, MA Wei min, WANG De ren, JIN Guang xing, LI Ji dong, YANG Yu e. Sequence Strata of Lower Cretaceous in Baiyinchagan Depression, Erlian Basin[J]. Acta Sedimentologica Sinica, 2004, 22(4): 644-650.
Citation: XU Shu tang, MA Wei min, WANG De ren, JIN Guang xing, LI Ji dong, YANG Yu e. Sequence Strata of Lower Cretaceous in Baiyinchagan Depression, Erlian Basin[J]. Acta Sedimentologica Sinica, 2004, 22(4): 644-650.
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