Zhang Tao, Yun Lu, Wu Xingwei, Ye Desheng. THE APPLICATION OF STRONTIUM ISOTOPES IN DIVISION OF PALEOKARST STAGES IN TAHE OIL FIELD[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2005, 27(3): 299-303. doi: 10.11781/sysydz200503299
Citation: Zhang Tao, Yun Lu, Wu Xingwei, Ye Desheng. THE APPLICATION OF STRONTIUM ISOTOPES IN DIVISION OF PALEOKARST STAGES IN TAHE OIL FIELD[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2005, 27(3): 299-303. doi: 10.11781/sysydz200503299

THE APPLICATION OF STRONTIUM ISOTOPES IN DIVISION OF PALEOKARST STAGES IN TAHE OIL FIELD

doi: 10.11781/sysydz200503299
  • Received Date: 2004-05-29
  • Rev Recd Date: 2005-03-08
  • Publish Date: 2005-05-25
  • Tahe oilfield is an Ordovician carbonate rock fissure vug oil pool which is mainly related to unconformity.Its reservoir rock is reformed by superimposition of multistages karstification,so it is very important to identify paleo-karstification stages and confirm distribution of different stage of karstfication reservoir for further exploration.Through recent years exploration,it is thought that the ratio of 87Sr/86Sr is an effective indicator distingishing middle Caledonian stage of karstification reservoir from early Hercynian stage of karstification reservoir.Its theory is that strontium isotope composition in the global ocean water at any one time in geologic history is homogeneous,that is,87Sr/86Sr value in ocean water changes timely.Combined with the geological setting that 87Sr/86Sr value in Caledonian stage of karstification reservoir is different from 87Sr/86Sr value in Hercynian stage of karstification reservoir and the experimental data,Pa-leokarstification reservoir stages is identified and predicted,and distribution pattern in Tahe oilfield is discussed in the paper,which provides geological evidence for further petroleum exploration in Tahe oilfield.

     

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  • [1]
    向芳,王成善.锶同位素在沉积学中的应用新进展[J].地质地球化学,2001,29(1):79~82
    [2]
    郑荣才,陈洪德,张哨楠.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-中国地质大学学报,1997,22(4):424~428
    [3]
    王敦则,黎玉战,俞仁连.塔里木盆地塔河油田下奥陶统油藏特征及成藏条件分析[J].石油实验地质,2003,25(2):122~128
    [4]
    顾忆.塔里木盆地北部塔河油田油气藏成藏机制[J].石油实验地质,2000,22(4):307~311
    [5]
    闫相宾,韩振华,李永宏.塔河油田奥陶系油藏的储层特征和成因机理探讨[J].地质论评,2002,48(6):619~626
    [6]
    王恕一.塔里木盆地塔河油田下奥陶统碳酸盐岩的深埋溶蚀作用及其对储集体的影响[J].石油实验地质,2003,25(增刊):557~561
    [7]
    蔡立国,钱一雄,刘光祥等.塔河油田及邻区地层水成因探讨[J].石油实验地质,2002,24(1):57~60
    [8]
    Wickman F E.Isotope rations:a clue to the age of certain marine sediments[J].Geol,1948,(56):61~66
    [9]
    Hodell D A,Mead G A,Mueller P A.Varition in the strontium isotopic composition of seawater (8Ma to present):implications for chemical weathering rates and dissolved fluxes to the ocaens[J].Chen Geo (Isot Geosci Sect),1990,(80):291~307
    [10]
    黄思静,石和,刘杰等.锶同位素地层学研究进展[J].地球科学进展,2001,16(2):194~200
    [11]
    Palmer MR,Elderfield H.Sr isotopic composition of sea water over the past 75 a[J].Naturre,1985,314:526~528
    [12]
    Raymo M E,Ruddiman W F.Tectonic forcingg of late Cenozonic climate[J].Nature,1992,359:117~122
    [13]
    刘文,李永宏,张涛.塔河油田奥陶系碳酸盐岩沉积相及地层学研究[J].石油实验地质,2002,24(2):104~109
    [14]
    叶德胜,王根长,林忠民等.塔里木盆地北部寒武-奥陶系碳酸盐岩储层特征及油气前景[M].成都:四川大学出版社,2000.50~51
    [15]
    马红强.盐水包裹体在成岩作用中的应用-以塔河油田下奥陶统碳酸盐岩为例[J].石油实验地质,2003,25(增刊):601~606
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