Advanced Search

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.
  • [1] 池英柳,张万选,李潍连, 等.白音查干凹陷有利勘探目标预测.断块油气田,1997,4(6):5~9[Chi Yingliu,Zhang Wanxuan,Li Weilian, et al. Evaluation of the Prospective Targets in the Baiyinchagan Sub-Basin. Fault-Block Oil and Gas Field, 1997,4(6):5~9]
    [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]
    [10] Timothy A.Cross.Stratigraphic controls on reservoir attributes in continental strata.Earth Science Frontiers (China University of Geosciences,Beijing),2000,7(4):322~350
    [11] 朱筱敏,王贵文,李滨阳, 等.开鲁盆地陆西凹陷下白垩统层序地层学和油气评价.沉积学报,2002,20(4):531~536[Zhu Xiaomin,Wang Guiwen,Li Binyang, et al. Lower Cretaceous sequence stratigraphy and hydrocarbon Evaluation in Kailu Basin. Acta Sedimentologica Sinica, 2002, 20(4): 531~536]
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(528) PDF downloads(1038) Cited by()

Proportional views
Related
Publishing history
  • 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.
Reference (11)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return