Advanced Search

Lai Zhiyun. CHARACTERISTICS OF MODERN DEPOSIT OF THE TAIPINGKOU DOWNSTREAM. POINT BAR OF 1'HE JINGZHOU REACH YANGTZE RIVER[J]. Acta Sedimentologica Sinica, 1986, 4(4): 109-118.
Citation: Lai Zhiyun. CHARACTERISTICS OF MODERN DEPOSIT OF THE TAIPINGKOU DOWNSTREAM. POINT BAR OF 1'HE JINGZHOU REACH YANGTZE RIVER[J]. Acta Sedimentologica Sinica, 1986, 4(4): 109-118.

CHARACTERISTICS OF MODERN DEPOSIT OF THE TAIPINGKOU DOWNSTREAM. POINT BAR OF 1'HE JINGZHOU REACH YANGTZE RIVER

  • Received Date: 1985-01-29
  • Publish Date: 1986-12-10
  • Along the south bank of the Yangtze river, between the Yuanshi bend and Shashi bend, there is a point bar which is named the Tai-Ping-Kou Downstream the Po-int Bar. Adjacent to it at the downstream, there is a channel bar(the Bar or Sanbatan), which is 7km in length and has an area of 7.5sq.km,Three-Eight with a nar-row fore and a wide tail, it appeares to be a planimetric form of wedge. A dinal ridge ranges all the way at both the fore and the tail.across the bar and there are some transversal longitu-furrows According to the 200m by 300m network, we have takes I05 samples on the surface of the bar sad dug 18 flutes(in depth of 1-2m).158 samples were used for the 19 for trace elements, 110 grain-size analysis, 6 for the clay mineral determination, for heavy minerals and 18 for the organic carbon dating.
  • [1] 成都地质学院陕北队,1976,沉积岩(物)粒度分析和应用,地质出版社,71-94页。
    [2] 刘宝用,1979,沉积岩石学,地质出版社,94-330页。
  • 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(513) PDF downloads(331) Cited by()

Proportional views
Related
Publishing history
  • Received:  1985-01-29
  • Published:  1986-12-10

CHARACTERISTICS OF MODERN DEPOSIT OF THE TAIPINGKOU DOWNSTREAM. POINT BAR OF 1'HE JINGZHOU REACH YANGTZE RIVER

Abstract: Along the south bank of the Yangtze river, between the Yuanshi bend and Shashi bend, there is a point bar which is named the Tai-Ping-Kou Downstream the Po-int Bar. Adjacent to it at the downstream, there is a channel bar(the Bar or Sanbatan), which is 7km in length and has an area of 7.5sq.km,Three-Eight with a nar-row fore and a wide tail, it appeares to be a planimetric form of wedge. A dinal ridge ranges all the way at both the fore and the tail.across the bar and there are some transversal longitu-furrows According to the 200m by 300m network, we have takes I05 samples on the surface of the bar sad dug 18 flutes(in depth of 1-2m).158 samples were used for the 19 for trace elements, 110 grain-size analysis, 6 for the clay mineral determination, for heavy minerals and 18 for the organic carbon dating.

Lai Zhiyun. CHARACTERISTICS OF MODERN DEPOSIT OF THE TAIPINGKOU DOWNSTREAM. POINT BAR OF 1'HE JINGZHOU REACH YANGTZE RIVER[J]. Acta Sedimentologica Sinica, 1986, 4(4): 109-118.
Citation: Lai Zhiyun. CHARACTERISTICS OF MODERN DEPOSIT OF THE TAIPINGKOU DOWNSTREAM. POINT BAR OF 1'HE JINGZHOU REACH YANGTZE RIVER[J]. Acta Sedimentologica Sinica, 1986, 4(4): 109-118.
Reference (2)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return