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古地理学报 ›› 2009, Vol. 11 ›› Issue (6): 689-696. doi: 10.7605/gdlxb.2009.06.009

• 古地理学及矿产资源 • 上一篇    下一篇

四川盆地东部上三叠统须家河组层序地层及聚煤特征研究*

高彩霞1,2 邵龙义1 李长林2 徐晓燕1 许海涛1   

  1. 1 中国矿业大学(北京)地球科学与测绘工程学院，北京 100083
    2 重庆地质矿产研究院，重庆 400042
  • 收稿日期:2009-06-02 修回日期:2009-07-27 出版日期:2009-12-01 发布日期:2009-12-01
  • 作者简介:高彩霞，女，现为中国矿业大学（北京）地球科学与测绘工程学院在读硕士生。
    通讯作者简介 邵龙义，男，现为中国矿业大学（北京）地球科学与测绘工程学院教授。
  • 基金资助:
    国家973项目(编号：2006CB202202)、国家油气重大专项（编号：2009ZX0509009-002）及国家自然科学基金项目(编号：40172050，40672103)联合资助

Sequence stratigraphy and coal accumulation of the Upper Triassic Xujiahe Formation in eastern Sichuan Basin

Gao Caixia1,2, Shao Longyi1, Li Changlin2, Xu Xiaoyan1, Xu Haitao1   

  1. 1 Gollege of Earth Sciences and Surveying Engineering，China University of Mining & Technology(Beijing)， Beijing 100083
    2 Chongqing Institute of Geology and Mineral Resources，Chongqing 400042
  • Received:2009-06-02 Revised:2009-07-27 Online:2009-12-01 Published:2009-12-01
  • About author:Gao Caixia is a master candidate of China University of Mining and Technology(Beijing).
    About the corresponding author Shao Longyi is a professor of China University of Mining and Technology (Beijing).

摘要： 四川盆地东部上三叠统须家河组共分7段，其中须一段与川西小塘子组为同期异相沉积。须一、须三、须五、须七段为含煤泥岩段，须二、须四、须六段为砂岩段。对区内钻井剖面及露头剖面进行分析，在须家河组中识别出区域性构造不整合面及河流下切冲刷面等层序界面，将须家河组划分为4个三级层序，分别对应于须一段、须二段—须三段、须四段—须五段、须六段—须七段。以地层的岩性、岩相变化特征细化分出低位体系域、湖侵体系域和高位体系域。其中低位体系域以广泛分布的河道砂岩沉积为特征；湖侵体系域与高位体系域以湖滨三角洲相的细砂岩、粉砂岩、泥岩及煤层互层为特征。对层序地层格架下的聚煤特征分析表明，层序Ⅲ聚煤最有利，其次为层序Ⅳ，层序Ⅱ最差；在层序Ⅲ内，高位体系域比湖侵体系域更有利于成煤。煤层厚度变化明显受泥炭堆积速率与可容空间增加速率的控制，高位体系域早期较高的可容空间增加速率与较高的泥炭堆积速率保持平衡，有利于厚泥炭(煤)层的形成。

关键词: 四川盆地东部, 层序地层, 聚煤作用, 须家河组

Abstract: The Xujiahe Formation of the Upper Triassic in the eastern Sichuan Basin is subdivided into seven members. The first member is correlated to the Xiaotangzi Formation of the western Sichuan Basin， but they have different facies. The first， third， fifth and seventh members are coal-bearing intervals， while the second， fourth and sixth members are sandstone-rich intervals. Four sequence boundaries represented by regional tectonic unconformities and the erosional base of the fluvial channel incised valley filling are recognized in the Xujiahe Formation based on outcrop and borehole data analysis. A total of four third-order sequences are subdivided in the Xujiahe Formation， and they are subcorrelated to the intervals of Member 1， Member 2 to Member 3， Member 4 to Member 5， and Member 6 to Member 7， respectively. Each sequence is further subdivided into lowstand systems tract(LST)， lacustrine transgressive systems tract(TST)and highstand systems tract(HST)according to variation in lithology and lithofacies. The LST is characterized by widely distributed channel sandstones， the TST and HST are featured with the lacustrine-deltaic interbedded fine sandstones， siltstones， mudstones and coals. The further analysis of coal accumulation in the sequence stratigraphic framework reveals that， sequence 3 is the most favorable sequence for coal accumulation，followed by sequence 4，sequence 2 is the worst. Within sequence 3， the coal-accumulation in HST is better than in the TST. Thickness of coal seams is controlled by the balance between the peat accumulation rate and the accumulation creation rate，and the thick coals tend to be formed in the early HST when the peat accumulation rate is well balanced with the accumulation creation rate.

Key words: eastern Sichuan Basin, sequence stratigraphy, coal accumulation, Xujiahe Formation

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