Advanced Search
Volume 28 Issue 4
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2006  >  28(4): 391-394
Hao Jianrong, Liu Yiqun, Cao Qing, Xing Xiujuan. THE STUDY OF FLUID INCLUSIONS IN JURASSIC OF THE SANTANGHU BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(4): 391-394. doi: 10.11781/sysydz200604391
Citation: Hao Jianrong, Liu Yiqun, Cao Qing, Xing Xiujuan. THE STUDY OF FLUID INCLUSIONS IN JURASSIC OF THE SANTANGHU BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(4): 391-394. doi: 10.11781/sysydz200604391
shu

THE STUDY OF FLUID INCLUSIONS IN JURASSIC OF THE SANTANGHU BASIN

doi: 10.11781/sysydz200604391
  • 1.

    State Key Laboratory of Continental Dynamics, Northwest University, Xi'an, Shaanxi 710069, China

  • 2. Department of Geology, Norhtwest University, Xi'an, Shaanxi 710069, China

  • Received Date: 2005-11-02
  • Rev Recd Date: 2006-06-24
  • Publish Date: 2006-07-28
    Abstract
  • Chosing the Santanghu Basin in Xinjiang as an example,according to secondary fluid inclusions' facieology,salinity,homogeny temperature and character of associated hydrocarbon fluid inclusions in Jurassic reservoir,it is believed that the inclusions in the crack of quartz have formed at different fluids process and of different periods combining with the study of thermal evolution of the basin.The analysis show that there exist a heat event at the end of Jurassic,migrating by cracks from the deep stratum.Accordingly,the fluid inclusions have great significance in analyzing of the information about hydrocarbon migration,at the same time,it can provide heat events in geological history.The fluid inclusions bear the characteristics of multi-origin and multi-period,which are critical in studying the thermal and maturity history of hydrocarbon source rocks in basin.

     

    • FullText(HTML)
  • loading
    • References(18)
  • [1]
    郑有业,李晓菊,马丽娟等.有机包裹体在生油盆地研究中的应用[J].地学前缘,1998,5(1-2):325～331
    [2]
    白国平.包裹体技术在油气勘探中的应用研究现状及发展趋势[J].石油大学学报(自然科学版),2002,27(4):136～140
    [3]
    孙樯,谢鸿森,郭捷.含油气沉积盆地流体包裹体及应用[J].长春科技大学学报,2000,30(1):42～45
    [4]
    王一刚,余晓锋,杨雨等.流体包裹体在建立四川盆地古地温剖面研究中的应用[J].地球科学,23(3):285～288
    [5]
    柳广弟,张仲培,张枝焕等.焉耆盆地三工河组储层流体包裹体形成期次分析[J].沉积学报,2002,20(2):345～348,353
    [6]
    赵靖舟,戴金星.库车前陆逆冲带天然气成藏期与成藏史[J].石油学报,2002,23(2):6～11
    [7]
    陶士振.包裹体应用于油气地质研究的前提条件和关键问题[J].地球科学,2004,39(1):77～91
    [8]
    陶士振,郭宏莉,张宝民等.沉积岩包裹体的岩相学、分类、术语及常被忽略的基本问题[J].地球科学,2003,38(2):275～280
    [9]
    周中毅,潘长春.沉积盆地古地温测定方法及其应用[M].广州:广东科技出版社,1992
    [10]
    孙自明,熊保贤,李永林等.三塘湖盆地构造特征与有利勘探方向[J].石油实验地质,2001,23(1):23～26
    [11]
    Robert H Goldstein.Fluid inclusions in sedimentary and diagenetic systems[J].Lithos,2001,55:159～193
    [12]
    侯建国,任丽华,董春梅.有机包裹体技术在油气运移与聚集中的应用研究[J].石油实验地质,2005,27(4):409～413
    [13]
    刘小平,徐健,杨立干.有机包裹体在油气运聚研究中的应用--以苏北盆地高邮凹陷为例[J].石油实验地质,2004,26(1):94～99
    [14]
    郝建荣,柳益群,冯乔等.新疆三塘湖盆地构造-热史研究[J].西北大学学报,2006,36(2):290～294
    [15]
    陈汉红,张启明,施继锡.琼东南盆地含烃热流体活动的流体包裹体证据[J].中国科学(D辑),1997,27(4):343～348
    [16]
    叶加仁,杨香华.沉积盆地热流体活动及其成藏动力学意义[J].沉积学报,2001,19(2):214～218
    [17]
    Roman E L,Coldhaber M B,Hatch J R.Regional fluid flow as a factor in the thermal history of the Illions Basin:constraints from inclusions and the maturity of Pennsylvanican coals[J].AAPG Bull,2002.86(2):257～277
    [18]
    刘建章,刘伟,王存武.沉积盆地活动热流体类型及其石油地质意义[J].海洋石油,2004,24(3):8～13
    • 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 (669) PDF downloads(333) 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