Advanced Search
Volume 33 Issue 4
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2011  >  33(4): 388-391
Zhang Liqiang, Luo Xiaorong. Distribution and characteristics of carbonate cements in overpressure zone of Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(4): 388-391. doi: 10.11781/sysydz201104388
Citation: Zhang Liqiang, Luo Xiaorong. Distribution and characteristics of carbonate cements in overpressure zone of Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(4): 388-391. doi: 10.11781/sysydz201104388
shu

Distribution and characteristics of carbonate cements in overpressure zone of Junggar Basin

doi: 10.11781/sysydz201104388
  • 1.

    School of Geosciences, China University of Petroleum, Qingdao, Shandong 266555, China

  • 2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

  • Received Date: 2011-04-11
  • Rev Recd Date: 2011-06-07
  • Publish Date: 2011-08-28
    Abstract
  • Based on studies of carbonate cement characteristics,the distribution and generation environment of carbonate cements in overpressure zone of the Paleogene Anjihaihe Formation in the southern margin of Junggar Basin have been discussed in this paper by means of thin section observation,well-logging interpretation and O-C isotope analysis.The carbonate cements in the study area are mainly composed of sparry ferri-calcite in connected-crystal form,characterized by low AC,high RT and low GR.Vertically,the cemented layers mainly locate in the pressure-released zone and the overpressure transition zone,including the upper and the lower parts of overpressure top surface,the top of sandstone belt in the overpressure zone as well as the lithologic transition belt in thick overpressure mudstone.Most of the carbonate cements have high negative oxygen isotope values.They were formed before or during petroleum migration under high temperature.

     

    • FullText(HTML)
  • loading
    • References(14)
  • [1]
    雷德文,唐勇,常秋生.准噶尔盆地南缘深部优质储集层及有利勘探领域[J].新疆石油地质,2008,29(4):435-438.
    [2]
    李耀华.准南前陆盆地油气成藏条件及有利勘探区[J].天然气工业,2002,22(S1):51-55.
    [3]
    李忠权,张寿庭,王洪辉,等.准噶尔盆地南缘构造成因机理及其与油气聚集关系探讨[J].成都理工学院学报,1997,24(2):4-6.
    [4]
    齐雪峰,吴晓智.准噶尔盆地南缘安集海河组沉积环境及油气地质意义[J].新疆石油地质,2009,30(3):289-292.
    [5]
    李忠权,陈更生,郭冀义,等.准噶尔盆地南缘西部地层异常高压基本地质特征[J].石油实验地质,2001,23(1):47-51.
    [6]
    查明,张卫海,曲江秀.准噶尔盆地异常高压特征、成因及勘探意义[J].石油勘探与开发,2000,27(2):31-35.
    [7]
    张闻林,张哨楠,陈义才,等.准南西部地层超压分析[J].天然气工业,2004,24(1):26-29.
    [8]
    王震亮,孙明亮,耿鹏,等.准南地区异常地层压力发育特征及形成机理[J].石油勘探与开发,2003,30(1):32-34.
    [9]
    罗晓容,肖立新,李学义,等.准噶尔盆地南缘中段异常压力分布及影响因素[J].地球科学——中国地质大学学报,2004,29(4):404-413.
    [10]
    陈丽华,姜再兴.储层实验测试技术[M].东营:石油大学出版社,1994:161-162.
    [11]
    Jansa L F,Noguera Urrea V H.Geology and diagenetic history of overpressured sandstone reservoirs,venture gas field,offshore Nova Scotia,Canada[J].AAPG Bulletin,1990,74(10):1640-1658.
    [12]
    郭宏莉,王大锐.塔里木油气区砂岩储集层碳酸盐胶结物的同位素组成与成因分析[J].石油勘探与开发,1999,26(3):31-35.
    [13]
    Irwin H,Curtis C,Coleman M L.Isotopic evidence for source of diagenetic carbonates for med during burial of organic-rich sediments[J].Nature,1977,269:209-213.
    [14]
    Hutcheon I,Abercrombie H J,Putnam P E,et al.Diagenesis and sedimentology of the Glearwater Formation at Tucker Lake[J].Bulletin of Canadian Petroleum Geology,1989,37(1):83-97.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 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
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (1796) PDF downloads(1028) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return