Chen Wanchuan, Hao Shumin, Huang Jiabin. CHARACTERISTICS AND FORMATIONAL MECHANISM OF THE SEDIMENT GRAVITY FLOW OF THE TANGWANG LING FORMATION OF SHAANXI[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1984, 6(3): 203-212. doi: 10.11781/sysydz198403203
Citation: Chen Wanchuan, Hao Shumin, Huang Jiabin. CHARACTERISTICS AND FORMATIONAL MECHANISM OF THE SEDIMENT GRAVITY FLOW OF THE TANGWANG LING FORMATION OF SHAANXI[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1984, 6(3): 203-212. doi: 10.11781/sysydz198403203

CHARACTERISTICS AND FORMATIONAL MECHANISM OF THE SEDIMENT GRAVITY FLOW OF THE TANGWANG LING FORMATION OF SHAANXI

doi: 10.11781/sysydz198403203
  • Received Date: 1983-11-02
  • Publish Date: 1984-07-25
  • The sediment gravity flow of the Tangwang Ling Formation can be divided into four types according to both their lithology and sedimentary characteristics, i.e., debris, clastic, grain and turbidity. This paper makes a statement on their characteristics, formational mechanism and development. The author suggests that the formation, development and distribution of the gravity flow of the Tangwang Ling Formation were under the effect of the second episode of the Caledonian and the control of differentiational uplift and subsidence faulting. Paleo-geographically it is referred as a residual ocean basin of foremountain faultdown type trending NEE. Sediments settled down by the gravity flow in this area are of the type of multiple-source faultdown-basin; the sediments were principally resulted from gravity flow in shallow water, rather than the so-called "glacial sediments".

     

  • loading
  • 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

    Article Metrics

    Article views (597) PDF downloads(345) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return