Advanced Search
Volume 27 Issue 3
. 
Turn off MathJax
Article Contents
Article Navigation >  Acta Sedimentologica Sinica  > 2009  >  27(3): 435-442

LIU Wei. Sedimentary Environment of LowerMiddle OrdovicianYingshan Formation in MidWestern Tarim Basin[J]. Acta Sedimentologica Sinica, 2009, 27(3): 435-442.
Citation: LIU Wei. Sedimentary Environment of LowerMiddle OrdovicianYingshan Formation in MidWestern Tarim Basin[J]. Acta Sedimentologica Sinica, 2009, 27(3): 435-442.
shu

Sedimentary Environment of LowerMiddle OrdovicianYingshan Formation in MidWestern Tarim Basin

  • Research Institute of Petroleum Exploration and Development, Beijing 100083

More Information
  • Corresponding author: LIU Wei
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2009-06-10
  • The time equivalent Yingshan Formation in Tarim Basin has been discussed. Based on this, the sedimentary environment of Yingshan Formation was reconstructed, with the aid of outcrops, seismic facies, strata contour map and core analysis, and draw three conclusions as follows: ①The distribution characteristic of platform edge at Daobaowanian Stage and Dawanian Stage and the type of platform were definite. Besides, the viewpoint that the discontinuity of reef and beach along the platform edge was put forward. ②Carbonate sands are wild range and the shape is multifarious. Generally, they are elongate or elliptical and strike of sands is parallel to the platform edge. ③The existence of intrashelf basin was proved. Along the edge of intrashelf basin there are carbonate sands and bioherm, generally sands on windward side and bioherm on lee side. In intrashelf basin sediments predominatly consist of pelagic carbonates, which are commonly rich in organic content.
  • 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(1657) PDF downloads(612) Cited by()

Proportional views
Related
Publishing history
  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2009-06-10

Sedimentary Environment of LowerMiddle OrdovicianYingshan Formation in MidWestern Tarim Basin

  • Research Institute of Petroleum Exploration and Development, Beijing 100083
    Corresponding author: LIU Wei
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2009-06-10

Abstract: The time equivalent Yingshan Formation in Tarim Basin has been discussed. Based on this, the sedimentary environment of Yingshan Formation was reconstructed, with the aid of outcrops, seismic facies, strata contour map and core analysis, and draw three conclusions as follows: ①The distribution characteristic of platform edge at Daobaowanian Stage and Dawanian Stage and the type of platform were definite. Besides, the viewpoint that the discontinuity of reef and beach along the platform edge was put forward. ②Carbonate sands are wild range and the shape is multifarious. Generally, they are elongate or elliptical and strike of sands is parallel to the platform edge. ③The existence of intrashelf basin was proved. Along the edge of intrashelf basin there are carbonate sands and bioherm, generally sands on windward side and bioherm on lee side. In intrashelf basin sediments predominatly consist of pelagic carbonates, which are commonly rich in organic content.

LIU Wei. Sedimentary Environment of LowerMiddle OrdovicianYingshan Formation in MidWestern Tarim Basin[J]. Acta Sedimentologica Sinica, 2009, 27(3): 435-442.
Citation: LIU Wei. Sedimentary Environment of LowerMiddle OrdovicianYingshan Formation in MidWestern Tarim Basin[J]. Acta Sedimentologica Sinica, 2009, 27(3): 435-442.
shu

    HTML

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