Advanced Search
Volume 33 Issue 5
. 
Turn off MathJax
Article Contents
Article Navigation >  Acta Sedimentologica Sinica  > 2015  >  33(5): 972-982

YANG XueFei, WANG XingZhi, TANG Hao, JIANG Nan, YANG YueMing, XIE JiRong, LUO WenJun. Research Sedimentary Microfacies of the Longwangmiao Formation in Moxi Area, Central Sichuan Basin[J]. Acta Sedimentologica Sinica, 2015, 33(5): 972-982. doi: 10.14027/j.cnki.cjxb.2015.05.013
Citation: YANG XueFei, WANG XingZhi, TANG Hao, JIANG Nan, YANG YueMing, XIE JiRong, LUO WenJun. Research Sedimentary Microfacies of the Longwangmiao Formation in Moxi Area, Central Sichuan Basin[J]. Acta Sedimentologica Sinica, 2015, 33(5): 972-982. doi: 10.14027/j.cnki.cjxb.2015.05.013
shu

Research Sedimentary Microfacies of the Longwangmiao Formation in Moxi Area, Central Sichuan Basin

doi: 10.14027/j.cnki.cjxb.2015.05.013
  • 1.

    State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610500;

  • 2.

    School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500;

  • 3.

    Research Institute of Exploration and Development, Southwest Oil and Gas Field Company, PetroChina, Chengdu 610051

  • Received Date: 2014-05-27
  • Rev Recd Date: 2014-11-23
  • Publish Date: 2015-10-10
  • Combined with the depositional background of Early Cambrian Longwangmiao Formation in Sichuan Basin, the lithology, sedimentary structures, logging response, microfacies and sedimentary evolution of Longwangmiao Formation in Moxi area were analyzed. It is indicated that in Longwangmiao period, the Moxi area was located in the restricted platform, and the Longwangmiao Formation was composed of dolarenites and crystalline dolomites deposited in the restricted lagoon and grain shoal. Vertically, Longwangmiao Formation was composed of two sets of up-shallowing deposition, from restricted lagoon to the grain shoals. Grain shoal can be subdivided into shoal core, shoal margin and inter-shoal low according to the lithology, sedimentary structures, cumulative thickness of grain dolomite and the grain dolomite thickness of the single shoal. Horizontally, the sedimentary distribution of the Upper Longwangmiao Formation is similar to that of the Lower Longwangmiao Formation, but the shoal scale had been larger with the eastward migration trends. The microfacies distribution is controlled by the palaeogeography characteristic and relative sea-level. The sedimentary evolution model of Longwangmiao Formation in Moxi area has been established.
  • 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(667) PDF downloads(456) Cited by()

Proportional views
Related
Publishing history
  • Received:  2014-05-27
  • Revised:  2014-11-23
  • Published:  2015-10-10

Research Sedimentary Microfacies of the Longwangmiao Formation in Moxi Area, Central Sichuan Basin

doi: 10.14027/j.cnki.cjxb.2015.05.013
  • 1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu 610500;
  • 2. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500;
  • 3. Research Institute of Exploration and Development, Southwest Oil and Gas Field Company, PetroChina, Chengdu 610051
  • Received Date: 2014-05-27
  • Rev Recd Date: 2014-11-23
  • Publish Date: 2015-10-10

Abstract: Combined with the depositional background of Early Cambrian Longwangmiao Formation in Sichuan Basin, the lithology, sedimentary structures, logging response, microfacies and sedimentary evolution of Longwangmiao Formation in Moxi area were analyzed. It is indicated that in Longwangmiao period, the Moxi area was located in the restricted platform, and the Longwangmiao Formation was composed of dolarenites and crystalline dolomites deposited in the restricted lagoon and grain shoal. Vertically, Longwangmiao Formation was composed of two sets of up-shallowing deposition, from restricted lagoon to the grain shoals. Grain shoal can be subdivided into shoal core, shoal margin and inter-shoal low according to the lithology, sedimentary structures, cumulative thickness of grain dolomite and the grain dolomite thickness of the single shoal. Horizontally, the sedimentary distribution of the Upper Longwangmiao Formation is similar to that of the Lower Longwangmiao Formation, but the shoal scale had been larger with the eastward migration trends. The microfacies distribution is controlled by the palaeogeography characteristic and relative sea-level. The sedimentary evolution model of Longwangmiao Formation in Moxi area has been established.

YANG XueFei, WANG XingZhi, TANG Hao, JIANG Nan, YANG YueMing, XIE JiRong, LUO WenJun. Research Sedimentary Microfacies of the Longwangmiao Formation in Moxi Area, Central Sichuan Basin[J]. Acta Sedimentologica Sinica, 2015, 33(5): 972-982. doi: 10.14027/j.cnki.cjxb.2015.05.013
Citation: YANG XueFei, WANG XingZhi, TANG Hao, JIANG Nan, YANG YueMing, XIE JiRong, LUO WenJun. Research Sedimentary Microfacies of the Longwangmiao Formation in Moxi Area, Central Sichuan Basin[J]. Acta Sedimentologica Sinica, 2015, 33(5): 972-982. doi: 10.14027/j.cnki.cjxb.2015.05.013
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