Dong Rongxin. SEDIMENTARY CHARATERS OF BRAIDED AND LOW—SINUOSITY STREAMS IN SANDO FORMATION OF LOWER TERTIARY, NORTHERN JIANGSU PROVINCE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1987, 9(4): 374-384. doi: 10.11781/sysydz198704374
Citation: Dong Rongxin. SEDIMENTARY CHARATERS OF BRAIDED AND LOW—SINUOSITY STREAMS IN SANDO FORMATION OF LOWER TERTIARY, NORTHERN JIANGSU PROVINCE[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1987, 9(4): 374-384. doi: 10.11781/sysydz198704374

SEDIMENTARY CHARATERS OF BRAIDED AND LOW—SINUOSITY STREAMS IN SANDO FORMATION OF LOWER TERTIARY, NORTHERN JIANGSU PROVINCE

doi: 10.11781/sysydz198704374
  • Received Date: 1986-09-08
  • Publish Date: 1987-10-25
  • In the sediments of paieostreams,there are certain amount of rare mineral deposits,such as gold,diamond,uranium,platinum and monazite,etc.and some important oil/gas reservoirs as well.Therefore,it is practi-cally significant to study the ancient fluvial sediments.Up to the present,much analysis have been made on the sedimentation of the sinuous streams,but those on braided streams are not enough.Taking Lower Tertiary fluvial sedimentation in Sando Formation of Northern Jiangsu as an example,the characters of fluvial sedimentation,and the relation between braided streams and low-sinuosity streams are discus-sed in this paper.For the recognition of the sedimentary characters of such streams,especially of the characters in ancient stratigraphic profiles,the author of this paper establishes a typical profile as a model.

     

  • [1]
    成冶,1976.某地白垩系中的冲积相,地质科学,第4期. 337-351页.
    [2]
    任明远、王乃梁,1981,现代沉积环境概论,科学出版社.
    [3]
    陈昌明、黄家宽等,1982,中国东部第三纪裂谷盆地的沉积模式,中国科学院地质研究所论文集,141-159页,科学出版社.
    [4]
    严钦尚、张国栋等,1979,苏北金湖凹陷阜宁群的海侵和沉积环境,地质学报,第1期,74-83页.
    [5]
    Stur.M.M.,I966.Highand Low Sinupity Steam Deposits with Examples from the Devonian of Spitsbergen.lournal of Scdimcntary PctcrolohY,V.36,P.1102-1117.
  • Relative Articles

  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-082024-092024-102024-112024-122025-012025-022025-032025-032025-042025-052025-06051015202530
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 20.2 %FULLTEXT: 20.2 %META: 78.3 %META: 78.3 %PDF: 1.4 %PDF: 1.4 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 2.2 %其他: 2.2 %Prineville: 0.2 %Prineville: 0.2 %上海: 0.2 %上海: 0.2 %丽水: 0.2 %丽水: 0.2 %六安: 0.2 %六安: 0.2 %北京: 3.1 %北京: 3.1 %南京: 1.0 %南京: 1.0 %台州: 0.2 %台州: 0.2 %呼和浩特: 0.2 %呼和浩特: 0.2 %大庆: 0.5 %大庆: 0.5 %孝感: 0.2 %孝感: 0.2 %张家口: 6.0 %张家口: 6.0 %扬州: 0.2 %扬州: 0.2 %无锡: 0.2 %无锡: 0.2 %杭州: 1.0 %杭州: 1.0 %湖州: 0.5 %湖州: 0.5 %芒廷维尤: 60.2 %芒廷维尤: 60.2 %衢州: 0.7 %衢州: 0.7 %西宁: 20.2 %西宁: 20.2 %遵义: 0.2 %遵义: 0.2 %邯郸: 0.2 %邯郸: 0.2 %郑州: 0.5 %郑州: 0.5 %重庆: 0.2 %重庆: 0.2 %金华: 0.2 %金华: 0.2 %长沙: 0.2 %长沙: 0.2 %阿什本: 0.2 %阿什本: 0.2 %青岛: 0.2 %青岛: 0.2 %首尔: 0.2 %首尔: 0.2 %其他Prineville上海丽水六安北京南京台州呼和浩特大庆孝感张家口扬州无锡杭州湖州芒廷维尤衢州西宁遵义邯郸郑州重庆金华长沙阿什本青岛首尔

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

    Article Metrics

    Article views (725) PDF downloads(206) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return