Advanced Search
Volume 20 Issue 2
. 
Turn off MathJax
Article Contents
Article Navigation >  Acta Sedimentologica Sinica  > 2002  >  20(2): 229-237

YU YuanJiang, SUN JingMin, ZHU QingZhong, YANG Bing, SHEN JunShan, LIU XianBin, HAN ChunMing. Preliminary Research on the Mesozoic Lithofacies-Palaeogeography in the Chalangla Area, Qiangtang Basin, Northern Tibet[J]. Acta Sedimentologica Sinica, 2002, 20(2): 229-237.
Citation: YU YuanJiang, SUN JingMin, ZHU QingZhong, YANG Bing, SHEN JunShan, LIU XianBin, HAN ChunMing. Preliminary Research on the Mesozoic Lithofacies-Palaeogeography in the Chalangla Area, Qiangtang Basin, Northern Tibet[J]. Acta Sedimentologica Sinica, 2002, 20(2): 229-237.
shu

Preliminary Research on the Mesozoic Lithofacies-Palaeogeography in the Chalangla Area, Qiangtang Basin, Northern Tibet

  • 1.

    China University of geoscience, Beijing 100083;

  • 2.

    Instit ute of Petroleum Exploration and development Petrochina, Beijing 100083;

  • 3.

    Huabei Oilfield fift h Extraction factory, RenIiu Hebei 062552;

  • 4.

    Huabei Oilfield Research Instit ute, RenIiu Hebei 062552

  • Received Date: 2001-02-26
  • Rev Recd Date: 2001-06-04
  • Publish Date: 2002-04-10
  • For the first time, the paper systematically rebuilds the Mesozoic lithofacies and palaeogeography in the Chalangla area of Qiangtang Basin in Northern Tibet by using methods of stratigraphically dominant facies/subfacies and integrated analyses. This is on the basis of the measured sections and route geologic survey profiles as well as sedimentary facies analyses. Marine-continental transition facies were dominant in Late Triassic, forming regression sedimentary cycles and consequently developing delta facies, coastal facies, and littoral-neritic facies belt from NE towards SW. In the Middle Jurassic epoch developed neritic facies deposits, consequently delta-platform-neritic continental shelf facies occurred from NE towards SW and displayed in NWW～SEE direction. Twice marine transgression peaks occurred at J2 q Period and J2 b Period,and constituted two sedimentary cycles from marine ingression to regression. In the Late Jurassic epoch developed sea-continental transitional facies,which were delta, tidal flat, platform facies belts and displayed in NW～SE direction.In the Cretaceous period discrepancy in lithofacies and palaeogeography was present from the early to late. In the early stage developed platform edge shallow facies to restricted platform facies on the background of remnant sea, which formed the third marine transgression peak. After rapid overall swelling, in the late stage occurred alluvial fan-braided river facies sedimentary cycles made of red polyterrigenous molasse deposits with multi-source supplying. The Mesozoic provenance was mainly the central uplift belt in the north, and secondly the highland in the east and uplift region in the west. In the process of sedimentary evolution, sedimentary source areas were different in different geologic ages, and the terrain in general,was characteristic of being higher in north and east but lower in south and west.
  • [1] 1. 朱同兴。从弧后盆地到前陆盆地的沉积演化-以西藏北部羌塘中生代盆地分析为例[A].特提斯地质[C].北京:地质出版社，1999,23号:1～15 [Zhu Tongxing.Sedimentary Evolution from Back-arc to Foreland Basin: An Example from the Qiangtang Mesozoic Basin in Northern Xizang[A].Tethyan Geology[C].Beijing: Geological Publishing House,1999,No.23:1～15 ]

    2. 李勇，伊海生，王成善。青藏高原北部晚三叠世Epigondollella动物群的发现及其地质意义[J].地质论评，1999,45（4）:628 [Li Yong,Yi Haisheng,Wang Chengshan.The Discovery and its Geologic significance of Epigondollella fauna at late Triassic epoch in Northern Qinghai-Tibet Plateau[J].Geological Review,1999,45（4）:628 ]

    3. 王成善，刘志飞，王国芝等。新生代青藏高原三维古地形再造[J].成都理工学院学报，2000,27（1）:1～7 [Wang Chengshan,Liu Zhifei,Wang Guozhi,et al.Three Dimension Palaeotopographic Reconstruction in Cenozoic Qinghai-Tibet Plateau [J].Journal of Chengdu University of Technology,2000,27（1）:1～7]

    4. 彭勇民，刘家铎。西藏东部昌都地区三叠纪岩相古地理[J].古地理学报，1999,1（4）:26～34 [Peng Yongmin and Liu Jiaduo.Lithofacies Palaeogeography of Triassic in Changdu Region,Eastern Tibet [J].Journal of Palaeogeography.1999,1（4）:26～34]

    5. 蔚远江。藏北羌塘查郎拉地区中生代沉积相展布及有利岩相带预测[J].地学前缘，2000,7（3）:118 [Yu Yuanjiang.The Sedimentary Facies Distribution and Forecast for the Favorable Lithofacies Belts of Mesozoic-Cenozoic in Chalangla Area,Qiangtang,Northern Tibet [J].Earth Science Frontiers （China University of Geosciences,Beijing），2000,7（3）: 118]

    6. 蔚远江。藏北羌塘查郎拉地区中生代盆地沉积构造背景探讨[J].地学前缘，2000,7（4）:470～476 [Yu Yuanjiang.Discussion on the sedimentary tectonic setting of Mesozoic basin in Chalangla Area,Qiangtang,Northern Tibet[J].Earth Science Frontiers（China University of Geosciences,Beijing），2000,7（4）:470～476]

    7. 西藏自治区地质矿产局。西藏自治区区域地质志[M].北京:地质出版社，1993 [Bureau of Geology and Mineral Resources of Xizang Autonomous Region.Regional Geology of Xizang（Tibet） Autonomous Region[M].Beijing: Geological Publishing House,1993]

    8. 蒋忠锡。羌塘地区侏罗纪地层若干问题[A].青藏高原地质文集（3）[C].北京:地质出版社，1983.87～112 [Jiang Zhongxi.Some Problems on the Jurassic Stratigraphy of Qiangtang Region[A].Contribution to The Geology of The Qinghai-Xizang（Tibet） Plateau [C],No.3,Beijing: Geological Publishing House,1983,87～112 ]

    9. 刘桂芳等。西藏喜玛拉雅地区上侏罗统和下白垩统研究的新进展[A].地层古生物论文集（17）[C].北京:地质出版社，1987.143～166 [Liu Guifang and Wang Sien.A New Advance in Study of The Upper Jurassic and Lower Cretaceous of The Himalayas,Xizang（Tibet） [A].Professional Papers of Stratigraphy And Palaeontology[C],No.17,Beijing: Geological Publishing House,1987,143～166]

    10. 梁寿生等。藏北班戈地区海相北垩系[A].青藏高原地质文集（6）[C].北京:地质出版社，1983 [Liang Shousheng Xia Jinbao.Marine Cretaceous of Bain'goin Area,North Xizang（Tibet）[A].Contribution to The Geology of The Qinghai-Xizang（Tibet） Plateau [C],No.3,Beijing: Geological Publishing House,1983.181～193]

    11. 刘训等。青藏高原不同地体的地层、生物区系及沉积构造演化史-亚东-格尔木岩石圈地学断面综合研究[R].北京:地质出版社，1992 [Liu Xun,et al.Different Terrains' Stratum,Biologic Provincial Series and Evolution History of Sedimentation-structure in Qinghai-Xizang（Tibet） Plateau-Integrated Research on lithosphere Geological Sections from Yadong to Geermu[R].Beijing: Geological Publishing House,1992]

    12. 刘宝王君，曾允孚主编。岩相古地理基础和工作方法[M].北京:地质出版社，1985 [Liu Baojun,Zeng Yunfu.Elements in lithopalaeogeolography and its working methods[M].Beijing: Geological Publishing House,1985]

    13. 刘宝王君，余光明等。岩相古地理学教程[M].地矿部岩相古地理工作协作组，北京:地质出版社，1990 [Liu Baojun,Yu Guangming,et al.Lithopalaeogeolography Tutorial[M].Collaboration Group on Lithopalaeogeolography in the Ministry of Geology and Mineral Resources[M].Beijing: Geological Publishing House,1990]

    14. 曾允孚，夏文杰主编。沉积岩石学[M].北京:地质出版社，1989 [Zeng Yunfu,Xia Wenjie.Sedimentary Petrology [M].Beijing: Geological Publishing House,1989]
  • 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
Get Citation
PDF
XML

Article Metrics

Article views(217) PDF downloads(15) Cited by()

Proportional views
Related
Publishing history
  • Received:  2001-02-26
  • Revised:  2001-06-04
  • Published:  2002-04-10

Preliminary Research on the Mesozoic Lithofacies-Palaeogeography in the Chalangla Area, Qiangtang Basin, Northern Tibet

  • 1. China University of geoscience, Beijing 100083;
  • 2. Instit ute of Petroleum Exploration and development Petrochina, Beijing 100083;
  • 3. Huabei Oilfield fift h Extraction factory, RenIiu Hebei 062552;
  • 4. Huabei Oilfield Research Instit ute, RenIiu Hebei 062552
  • Received Date: 2001-02-26
  • Rev Recd Date: 2001-06-04
  • Publish Date: 2002-04-10

Abstract: For the first time, the paper systematically rebuilds the Mesozoic lithofacies and palaeogeography in the Chalangla area of Qiangtang Basin in Northern Tibet by using methods of stratigraphically dominant facies/subfacies and integrated analyses. This is on the basis of the measured sections and route geologic survey profiles as well as sedimentary facies analyses. Marine-continental transition facies were dominant in Late Triassic, forming regression sedimentary cycles and consequently developing delta facies, coastal facies, and littoral-neritic facies belt from NE towards SW. In the Middle Jurassic epoch developed neritic facies deposits, consequently delta-platform-neritic continental shelf facies occurred from NE towards SW and displayed in NWW～SEE direction. Twice marine transgression peaks occurred at J2 q Period and J2 b Period,and constituted two sedimentary cycles from marine ingression to regression. In the Late Jurassic epoch developed sea-continental transitional facies,which were delta, tidal flat, platform facies belts and displayed in NW～SE direction.In the Cretaceous period discrepancy in lithofacies and palaeogeography was present from the early to late. In the early stage developed platform edge shallow facies to restricted platform facies on the background of remnant sea, which formed the third marine transgression peak. After rapid overall swelling, in the late stage occurred alluvial fan-braided river facies sedimentary cycles made of red polyterrigenous molasse deposits with multi-source supplying. The Mesozoic provenance was mainly the central uplift belt in the north, and secondly the highland in the east and uplift region in the west. In the process of sedimentary evolution, sedimentary source areas were different in different geologic ages, and the terrain in general,was characteristic of being higher in north and east but lower in south and west.

YU YuanJiang, SUN JingMin, ZHU QingZhong, YANG Bing, SHEN JunShan, LIU XianBin, HAN ChunMing. Preliminary Research on the Mesozoic Lithofacies-Palaeogeography in the Chalangla Area, Qiangtang Basin, Northern Tibet[J]. Acta Sedimentologica Sinica, 2002, 20(2): 229-237.
Citation: YU YuanJiang, SUN JingMin, ZHU QingZhong, YANG Bing, SHEN JunShan, LIU XianBin, HAN ChunMing. Preliminary Research on the Mesozoic Lithofacies-Palaeogeography in the Chalangla Area, Qiangtang Basin, Northern Tibet[J]. Acta Sedimentologica Sinica, 2002, 20(2): 229-237.
shu

    HTML

Reference (1)

Catalog

    Links

    Journal Online

    Contact Us

    • Website Copyright © 2011 Editorial Office of Acta Sedimentologica Sinica
    • Address: 8 Tianshui Middle Road, Lanzhou
    • Post code: 730000   Tel:（0931）8264231
    • 陇ICP备2021001824号-28
    • 甘公网安备 62010202000673号
    Wechat

    Email alert

    RSS

    Supported by: Beijing Renhe Information Technology Co. Ltd  

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return