Advanced Search
Turn off MathJax
Article Contents

Variation of the drainage density of Golmud fan in Qaidam Basin[J]. Acta Sedimentologica Sinica. doi: 10.14027/j.issn.1000-0550.2024.082
Citation: Variation of the drainage density of Golmud fan in Qaidam Basin[J]. Acta Sedimentologica Sinica. doi: 10.14027/j.issn.1000-0550.2024.082

Variation of the drainage density of Golmud fan in Qaidam Basin

doi: 10.14027/j.issn.1000-0550.2024.082
  • Received Date: 2024-04-12
    Available Online: 2024-07-10
  • Abstract:[Objective] By studying the distribution law of river network plane of modern distributive fluvial system,the reservoir distribution of underground fluvial sand-bodies is predicted, which provides knowledge base for reservoir modeling and guides oil and gas exploration and development. [Methods] By using modern geographic information software such as Google Earth, Global Mapper and 91Satellite Map Assistant, the number and width of Golmud fluvial fan channels were collected according to equal interval survey lines, and the drainage density (Dw) of Golmud fluvial fan was calculated, and the variation of the drainage density of Golmud fluvial fan was summarized, and the main controlling factors of drainage density (Dw) were analyzed. [Results and Discussions] (1)Golmud fluvial fan can be roughly divided into three phases: proximal, middle and distal. The proximal drainage density (Dw) ranges from 0.089-0.198, and the average drainage density (Dw) is 0.143. The middle drainage density (Dw) ranges from 0.136-0.19, and the average drainage density (Dw) is 0.164. The distal drainage density (Dw) ranges from 0.16 to 0.37, and the average drainage density (Dw) is 0.25; (2) The main controlling factors of drainage density (Dw) are tectonic movement and geomorphic factor; (3) The difference of tectonic movement and geomorphic factor leads to the fluctuation of drainage density (Dw). On the contrary, different drainage density (Dw) can also be used to identify and restore underground palaeochanne and paleoenvironmental conditions, and guide oil and gas exploration and development. [Conclusions] The study of drainage density (Dw) of Golmud fluvial fan promotes the development of sedimentology in distributive fluvial systems, providing a new method for prediction of underground reservoir distribution, and provides a large amount of data for reservoir modeling knowledge base.
  • 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(100) PDF downloads(11) Cited by()

Proportional views
Related
Publishing history
  • Received:  2024-04-12

Variation of the drainage density of Golmud fan in Qaidam Basin

doi: 10.14027/j.issn.1000-0550.2024.082

Abstract: Abstract:[Objective] By studying the distribution law of river network plane of modern distributive fluvial system,the reservoir distribution of underground fluvial sand-bodies is predicted, which provides knowledge base for reservoir modeling and guides oil and gas exploration and development. [Methods] By using modern geographic information software such as Google Earth, Global Mapper and 91Satellite Map Assistant, the number and width of Golmud fluvial fan channels were collected according to equal interval survey lines, and the drainage density (Dw) of Golmud fluvial fan was calculated, and the variation of the drainage density of Golmud fluvial fan was summarized, and the main controlling factors of drainage density (Dw) were analyzed. [Results and Discussions] (1)Golmud fluvial fan can be roughly divided into three phases: proximal, middle and distal. The proximal drainage density (Dw) ranges from 0.089-0.198, and the average drainage density (Dw) is 0.143. The middle drainage density (Dw) ranges from 0.136-0.19, and the average drainage density (Dw) is 0.164. The distal drainage density (Dw) ranges from 0.16 to 0.37, and the average drainage density (Dw) is 0.25; (2) The main controlling factors of drainage density (Dw) are tectonic movement and geomorphic factor; (3) The difference of tectonic movement and geomorphic factor leads to the fluctuation of drainage density (Dw). On the contrary, different drainage density (Dw) can also be used to identify and restore underground palaeochanne and paleoenvironmental conditions, and guide oil and gas exploration and development. [Conclusions] The study of drainage density (Dw) of Golmud fluvial fan promotes the development of sedimentology in distributive fluvial systems, providing a new method for prediction of underground reservoir distribution, and provides a large amount of data for reservoir modeling knowledge base.

Variation of the drainage density of Golmud fan in Qaidam Basin[J]. Acta Sedimentologica Sinica. doi: 10.14027/j.issn.1000-0550.2024.082
Citation: Variation of the drainage density of Golmud fan in Qaidam Basin[J]. Acta Sedimentologica Sinica. doi: 10.14027/j.issn.1000-0550.2024.082

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return