Advanced Search
Volume 28 Issue 3
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2006  >  28(3): 201-205
Liu Yunsheng, Guo Zhanfeng, Liang Xiwen, Yang Zhenwu. TECTONIC SIGNIFICANCE OF SANDSTONES AND COUPLING RELATION OF BASIN AND MOUNTAIN IN THE LATETRIASSIC-JURASSIC IN THE MIDDLE AND UPPER YANGTZE REGION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(3): 201-205. doi: 10.11781/sysydz200603201
Citation: Liu Yunsheng, Guo Zhanfeng, Liang Xiwen, Yang Zhenwu. TECTONIC SIGNIFICANCE OF SANDSTONES AND COUPLING RELATION OF BASIN AND MOUNTAIN IN THE LATETRIASSIC-JURASSIC IN THE MIDDLE AND UPPER YANGTZE REGION[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(3): 201-205. doi: 10.11781/sysydz200603201
shu

TECTONIC SIGNIFICANCE OF SANDSTONES AND COUPLING RELATION OF BASIN AND MOUNTAIN IN THE LATETRIASSIC-JURASSIC IN THE MIDDLE AND UPPER YANGTZE REGION

doi: 10.11781/sysydz200603201
  • 1.

    China University of Mining Technology, Beijing 100083, China

  • 2. Exploration & Development Research Institute of Jianghan Oilfield Branch Company, SINOPEC, Qianjiang, Hubei 433124, China

  • Received Date: 2005-10-21
  • Rev Recd Date: 2006-03-31
  • Publish Date: 2006-05-28
    Abstract
  • Based on the sandstone clastic model built by Dickinson et al,the characteristics of detrital composition of the Late Triassic-Jurassic sandstones in the Middle and Upper Yangtze region are studied to determine the types of source areas.It is presented that the main provenances of the Late Triassic-Jurassic basin comes from the East Qinling and Dabie orogenic belt,Longmenshan mountain and Jiangnan obduction zone.The main types of provenances attribute to the properties of recycled orogenic belt.The variational sequences of detrital compositions are the sedimentary responses to the three times of obduction of orogenic belt in the surrounding margin of basin.The analysis on the tectonic significance of detrital composition of the Late Triassic-Jurassic sandstones shows that the Late Triassic-Jurassic basin in the southern margin of the East Qinling and Dabie orogenic belt is a foreland basin located in the foreland of a collision orogen and thrusting nappe belt.The coupling relations of basin and mountain and Mesozoic tectonic evolution in the East Qinling and Dabie orogenic belt were also discussed in this paper.

     

    • FullText(HTML)
  • loading
    • References(14)
  • [1]
    张国伟,张本仁,袁学诚等.秦岭造山带与大陆动力学[M].北京:科学出版社,2001.1～835
    [2]
    殷鸿福,张克信.中央造山带的演化及其特点[J].地球科学,1998,23(5):438～442
    [3]
    高长林,刘光祥,张玉箴等.东秦岭-大巴山逆冲推覆构造与油气远景[J].石油实验地质,2003,25(增刊):523～531,538
    [4]
    汤加富,周存亭,侯明金等.大别山及邻区地质构造特征与形成演化[M].北京:地质出版社,2003.198～235
    [5]
    吉让寿,高长林,秦德余.华北与扬子两板块的拼贴方式与扬子北缘古生代盆地应变特征[J].石油实验地质,2004,26(2):143～152
    [6]
    范小林,陈浙春.东秦岭-大别造山带两侧盆地深部过程及古生界油气前景——以川东北盆地和合肥盆地为例[J].石油实验地质,2005,27(4):338～345
    [7]
    Dickinson W R,Suczek C A.Plate tectonics and sandstone compositions[J].AAPG Bulletin,1979,94(2):2164～2182
    [8]
    Dickinson W R,Beard L S,Brakenridge G R,et al.Provenance of North American Phanerozoic sandstone in relation to tectonic setting[J].Geol Soc Amer Bull,1983,94(2):222～235
    [9]
    李忠,李任伟,孙枢等.大别山南麓中生代盆地充填记录对造山作用属性的反映[J].中国科学(D辑),2002,32(6):469～478
    [10]
    汪泽成,赵文智,张林等.四川盆地构造层序与天然气勘探[M].北京:地质出版社,2002.3～94
    [11]
    许效松,刘宝珺,徐强等.中国西部大型盆地分析及地球动力学[M].北京:地质出版社,1997.16～38
    [12]
    吉让寿,高长林.秦岭-大别造山带两侧中新生代构造变格与成盆作用[J].石油实验地质,2005,27(5):449～454
    [13]
    刘少峰,张国伟,程顺有等.东秦岭-大别及邻区挠曲类盆地与碰撞造山过程[J].地质科学,1999,34(2):336～346
    [14]
    Flemings P B,Jordan T E.Stratigraphic modeling of foreland basins:interpreting thrust deformation and lithosphere rheology[J].Geology,1990,18:430 ～ 434
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    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
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (852) PDF downloads(385) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return