Advanced Search
Volume 26 Issue 2
. 
Turn off MathJax
Article Contents
Abstract
References
Article Navigation >  Acta Sedimentologica Sinica  > 2008  >  26(2): 221-233

REN Fenglou. The Prototype Character of Jiaolai Basin in Cretaceous Laiyang Period[J]. Acta Sedimentologica Sinica, 2008, 26(2): 221-233.
Citation: REN Fenglou. The Prototype Character of Jiaolai Basin in Cretaceous Laiyang Period[J]. Acta Sedimentologica Sinica, 2008, 26(2): 221-233.
shu

The Prototype Character of Jiaolai Basin in Cretaceous Laiyang Period

  • Exploration Item Management Department,Shengli Oil Field, Dongying Shandong 257015)

More Information
  • Corresponding author: REN Fenglou
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2008-04-10
  • Laiyang Formation of Jiaolai Basin is the target stratum for oil and gas exploration. By measuring several field sections, log datum, seismic datum paleocurrent direction,the paper indicated that different structural locations have different sedimentary facies. The Authors constructed sedimentary framework of Laiyang formation. Further more found two subside and deposition center, one is called ZhuwuJimo sag, along NNE direction, controlled by MupingJimo fault belt, another is called JuxianZhucheng sag, also NNE direction, along Shuriver rift and Zhucheng depression. Two sags is a relatively independent sedimentary unit in Laiyang period. The two sags dominated sedimentary formwork in Laiyang Formation period, Shuinan member was apex of lake development, mainly was lacustrine facieses. While Qugezhuang member, mainly was alluvial deposition. North border fault activity of Sulu Oregon belt controlled the Laiyang Formation deposition.
  • Created with Highcharts 5.0.7Amount of accessChart context menuAbstract Views, HTML Views, PDF Downloads StatisticsAbstract ViewsHTML ViewsPDF Downloads2024-072024-082024-092024-102024-112024-122025-012025-022025-032025-042025-052025-0602.557.51012.5
    Created with Highcharts 5.0.7Chart context menuAccess Class DistributionFULLTEXT: 9.8 %FULLTEXT: 9.8 %META: 82.7 %META: 82.7 %PDF: 7.5 %PDF: 7.5 %FULLTEXTMETAPDF
    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 5.6 %其他: 5.6 %其他: 1.4 %其他: 1.4 %China: 0.2 %China: 0.2 %United States: 1.2 %United States: 1.2 %上海: 1.4 %上海: 1.4 %东营: 0.5 %东营: 0.5 %中卫: 1.2 %中卫: 1.2 %乌海: 0.2 %乌海: 0.2 %兰州: 0.2 %兰州: 0.2 %凉山: 0.2 %凉山: 0.2 %北京: 10.7 %北京: 10.7 %南京: 0.2 %南京: 0.2 %南平: 0.5 %南平: 0.5 %呼和浩特: 0.2 %呼和浩特: 0.2 %哈尔滨: 0.2 %哈尔滨: 0.2 %大连: 0.2 %大连: 0.2 %天津: 0.5 %天津: 0.5 %宝鸡: 0.2 %宝鸡: 0.2 %宣城: 0.2 %宣城: 0.2 %山景城: 0.7 %山景城: 0.7 %巴彦淖尔: 0.2 %巴彦淖尔: 0.2 %张家口: 2.1 %张家口: 2.1 %惠州: 0.2 %惠州: 0.2 %成都: 0.5 %成都: 0.5 %扬州: 0.5 %扬州: 0.5 %武汉: 0.2 %武汉: 0.2 %沈阳: 0.2 %沈阳: 0.2 %济宁: 2.3 %济宁: 2.3 %淮北: 0.2 %淮北: 0.2 %深圳: 0.2 %深圳: 0.2 %温哥华: 0.2 %温哥华: 0.2 %湖州: 0.7 %湖州: 0.7 %漯河: 0.5 %漯河: 0.5 %烟台: 0.5 %烟台: 0.5 %牡丹江: 0.2 %牡丹江: 0.2 %石家庄: 0.2 %石家庄: 0.2 %芒廷维尤: 24.8 %芒廷维尤: 24.8 %芝加哥: 0.2 %芝加哥: 0.2 %苏州: 0.5 %苏州: 0.5 %蚌埠: 0.2 %蚌埠: 0.2 %衢州: 0.2 %衢州: 0.2 %西宁: 34.6 %西宁: 34.6 %西安: 0.5 %西安: 0.5 %贵阳: 0.2 %贵阳: 0.2 %运城: 0.2 %运城: 0.2 %郑州: 0.5 %郑州: 0.5 %重庆: 0.5 %重庆: 0.5 %长沙: 0.2 %长沙: 0.2 %青岛: 2.3 %青岛: 2.3 %其他其他ChinaUnited States上海东营中卫乌海兰州凉山北京南京南平呼和浩特哈尔滨大连天津宝鸡宣城山景城巴彦淖尔张家口惠州成都扬州武汉沈阳济宁淮北深圳温哥华湖州漯河烟台牡丹江石家庄芒廷维尤芝加哥苏州蚌埠衢州西宁西安贵阳运城郑州重庆长沙青岛
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(1855) PDF downloads(629) Cited by()

Proportional views
Related
Publishing history
  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2008-04-10

The Prototype Character of Jiaolai Basin in Cretaceous Laiyang Period

  • Exploration Item Management Department,Shengli Oil Field, Dongying Shandong 257015)
    Corresponding author: REN Fenglou
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2008-04-10

Abstract: Laiyang Formation of Jiaolai Basin is the target stratum for oil and gas exploration. By measuring several field sections, log datum, seismic datum paleocurrent direction,the paper indicated that different structural locations have different sedimentary facies. The Authors constructed sedimentary framework of Laiyang formation. Further more found two subside and deposition center, one is called ZhuwuJimo sag, along NNE direction, controlled by MupingJimo fault belt, another is called JuxianZhucheng sag, also NNE direction, along Shuriver rift and Zhucheng depression. Two sags is a relatively independent sedimentary unit in Laiyang period. The two sags dominated sedimentary formwork in Laiyang Formation period, Shuinan member was apex of lake development, mainly was lacustrine facieses. While Qugezhuang member, mainly was alluvial deposition. North border fault activity of Sulu Oregon belt controlled the Laiyang Formation deposition.

REN Fenglou. The Prototype Character of Jiaolai Basin in Cretaceous Laiyang Period[J]. Acta Sedimentologica Sinica, 2008, 26(2): 221-233.
Citation: REN Fenglou. The Prototype Character of Jiaolai Basin in Cretaceous Laiyang Period[J]. Acta Sedimentologica Sinica, 2008, 26(2): 221-233.
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