Advanced Search
Volume 31 Issue 3
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2009  >  31(3): 270-274
Liu Xianfeng, Cai Zhongxian, Yun Lu, Xu Wei. ELEMENT GEOCHEMISTRY CHARACTERISTIC RESPONSE FOR KARSTIFICATION IN THE TAHE OILFIELD[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(3): 270-274. doi: 10.11781/sysydz200903270
Citation: Liu Xianfeng, Cai Zhongxian, Yun Lu, Xu Wei. ELEMENT GEOCHEMISTRY CHARACTERISTIC RESPONSE FOR KARSTIFICATION IN THE TAHE OILFIELD[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2009, 31(3): 270-274. doi: 10.11781/sysydz200903270
shu

ELEMENT GEOCHEMISTRY CHARACTERISTIC RESPONSE FOR KARSTIFICATION IN THE TAHE OILFIELD

doi: 10.11781/sysydz200903270
  • 1.

    China University of Geosciences, Faculty of Resources, Wuhan, Hubei 430074, China

  • 2. China University of Geosciences, Graduate School, Wuhan, Hubei 430074, China

  • 3. China University of Geosciences, Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, Wuhan, Hubei 430074, China

  • 4. Design and Planning Institute of Northwest Petroleum Bureau, SINOPEC, Urumqi, Xinjiang 830011, China

  • 5. Exploration Research Dept.CNOOC Research, Beijing 100027, China

  • Received Date: 2008-03-16
  • Rev Recd Date: 2009-04-02
  • Publish Date: 2009-06-28
    Abstract
  • The Tahe Oilfield is located in the southwest margin of Akekule Uplift in north Tarim Basin.It went through several times tectonic uplift from the late Caledonian to the early Hercynian,this lead to Ordovician carbonate formation be exposed to the surface for a long time and suffering from intense air fresh-water weathering,leaching and dissolving and developed a set of complicated superficial karst system.Throuth research of arenaceous and pelitic karstic cave deposit about its' trace element such as B,V,Ga,Rb,etc,and REE characteristic in the main region of the Tahe Oilfield,it indicated that most samples took on characteristic of fresh-water corrosion.While,samples of the four wells such as T615 showed influenced by seawater,it can be indicated that seawater-freshwater mixing corrosion caused by widely marine transgression in early of Carboniferous Period probably overlay and improved the Ordovician karst system in the Tehe Oilfield.

     

    • FullText(HTML)
  • loading
    • References(30)
  • [1]
    饶丹,马绪杰,贾存善等.塔河油田主体区奥陶系缝洞系统与油气分布[J].石油实验地质,2007,29(6):589～592
    [2]
    肖玉茹,何峰煜,孙义梅.古洞穴型碳酸盐岩储层特征研究:以塔河油田奥陶系古洞穴为例[J].石油与天然气地质,2003,24(1):75～80
    [3]
    陈强路,何治亮,李思田.塔中地区奥陶系碳酸盐岩储层与油气聚集带[J].石油实验地质,2007,29(4):367～372
    [4]
    阎相宾.塔河油田奥陶系碳酸盐岩储层特征[J].石油与天然气地质,2002,23(3):262～265
    [5]
    康玉柱.塔里木盆地古生代海相碳酸盐岩储集岩特征[J].石油实验地质,2007,29(3):217～223
    [6]
    郭建华.塔北、塔中地区下古生界深埋藏古岩溶[J].中国岩溶,1996,15(3):207～216
    [7]
    袁道先.岩溶学词典[M].北京:地质出版社,1988
    [8]
    刘小平,吴欣松,张祥忠.轮古西地区奥陶系碳酸盐岩古岩溶储层碳、氧同位素地球化学特征[J].西安石油大学学报,2004,19(4):69～76
    [9]
    张云峰,王清晨.济阳坳陷奥陶系碳酸盐岩及缝洞充填方解石C、O同位素特征及其意义[J].地质科学,2007,42(3):570～578
    [10]
    舒勇,郑永飞,魏春生.白云鄂博碳酸岩墙碳氧同位素地球化学[J].地球化学,2001,30(2):169～175
    [11]
    王大瑞,白自强.广西及邻区泥盆系碳酸盐岩碳氧同位素组成特征及意义[J].北京大学学报,1995,31(4):460～466
    [12]
    黄思静,刘树根,李国蓉.奥陶系海相碳酸盐锶同位素组成及受成岩流体的影响[J].成都理工大学学报,2004,30(1):1～7
    [13]
    刘存革,李国蓉,张一伟.锶同位素在古岩溶研究中的应用:以塔河油田奥陶系为例[J].地质学报,2007,81(10):1398～1406
    [14]
    夏日元,唐建生,邹胜章等.塔里木盆地北缘古岩溶充填物包裹体特征[J].中国岩溶,2006,25(3):246～249
    [15]
    刘刚,周东升.微量元素分析在判别沉积环境中的应用:以江汉盆地潜江组为例[J].石油实验地质.2007,29(3):307～314
    [16]
    郑荣才,陈洪德,张哨楠等.川东黄龙组古岩溶储层的稳定同位素和流体性质[J].地球科学,1997,2 2(4):424～428
    [17]
    郑荣才,陈洪德.川东黄龙组古岩溶储层微量和稀土元素地球化学特征[J].成都理工学院学报,1997,24(1):1～7
    [18]
    杨守业,李从先.REE示踪沉积物物源研究进展[J].地球科学进展,1999,14(2):164～167
    [19]
    Potter P E,Shimp N F,Witters J.Trace elements in marine and fresh-water argillaceous sediments[J].Geochimica et Cosmochimica Acta,1963,27:669～694
    [20]
    赵振华.微量元素地球化学原理[M].北京:科学出版社,1997
    [21]
    刘宝珺.岩相古地理基础和工作方法[M].北京:地质出版社,1985
    [22]
    张金亮.塔里木盆地志留系古海洋沉积环境的元素地球化学特征[J].中国海洋大学学报,2006,36(2):200～208
    [23]
    戴塔根.应用地球化学[M].长沙:中南大学出版社,2005
    [24]
    Degens E T,Williams E G,Keith M L.Application of geochemical criteria[Pennsylvania],Part 2 of environmental stu-dies of Carboniferous sediments[J].AAPG Bulletin,1958,42:981～997
    [25]
    严钦尚,张国栋,顶立蒿等.苏北金湖凹陷阜宁群的海侵和沉积环境[J].地质学报,1979,(1):74～83
    [26]
    彭海艳,陈洪德.微量元素分析在沉积环境识别中的应用[J].新疆地质,2006,2(2):202～205
    [27]
    陈衍景.环境对沉积物微量元素含量和配分型式的制约[J].地质地球化学,1996,3 (97):97～105
    [28]
    Taylor S R,McLennan S M.The continental crust:Its composition and evolution:an examination of the geochemical record preserved in sedimentary rocks[M].Oxford:Blackwell Scientific Pub,1985.312
    [29]
    韩吟文,马振东.地球化学[M].北京:地质出版社,2003
    [30]
    强子同.碳酸盐岩储层地质学[M].东营:中国石油大学出版社,2007
    • 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 (1320) PDF downloads(991) 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