Yu Renlian. CHARACTERISTICS AND SIGNIFICANCE OF THE CALEDONIAN KARST IN THE TAHE OIL FIELD, THE TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2005, 27(5): 468-472. doi: 10.11781/sysydz200505468
Citation: Yu Renlian. CHARACTERISTICS AND SIGNIFICANCE OF THE CALEDONIAN KARST IN THE TAHE OIL FIELD, THE TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2005, 27(5): 468-472. doi: 10.11781/sysydz200505468

CHARACTERISTICS AND SIGNIFICANCE OF THE CALEDONIAN KARST IN THE TAHE OIL FIELD, THE TARIM BASIN

doi: 10.11781/sysydz200505468
  • Received Date: 2005-05-03
  • Rev Recd Date: 2005-07-01
  • Publish Date: 2005-09-25
  • The Tahe oil field is located in the Akekule uplift in the north of Tarim basin.It is the biggest carbonate hydrocarbon reservoir found in the Tarim basin up to now,and the biggest in China.According to exploration,the Ordovician reservoir,as the main reservoir bed in Tahe oil field,is mainly composed of hole,cave and aperture.Karst development consequentially controls the development of carbonate aperture-cave reservoir and reservoir formation.Kinds of data indicate that,there is Caledonian,besides Hercynian karst in the Tahe oil field.Study findings indicate that,native rock characteristics,development of rupture and fissure,ancient physiognomy,climate and water system control karst development,among which ancient physiognomy and development of rupture and fissure are the main factors.The Caledonian karst plays an important role in the development of rupture and fissure system of Ordovician carbonate rock,and is important to the exploration of middle Ordovician Yijianfang Formation,middle-low Ordovician Yinshan Formation and upper Ordovician Lianglitage Formation covered by the upper Ordovician Sangtamu Formation,consequentially enlarging the exploration foreground in this area.

     

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  • [1]
    黎玉战.塔里木盆地塔河油田发现历程及其意义[J].石油实验地质,2004,26(2):180~186.
    [2]
    周玉琦.塔里木盆地塔河油田的勘探实践与认识[J].石油实验地质,2001,23(4):363~367.
    [3]
    王恕一.塔里木盆地塔河油田下奥陶统碳酸盐岩的空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):601~606.
    [4]
    翟晓先.塔里木盆地北部复杂地质条件下寻找大油气田的方向和地区[A].见:康玉柱编.中国塔里木盆地石油地质文集[C].北京:地质出版社,1996.
    [5]
    张光亚,宋建国.塔里木克拉通盆地改造对油气聚集和保存的控制[J].地质论评,1998,44(5):511~521.
    [6]
    何发岐.塔里木盆地塔河油田近年来勘探主要成果与下一步勘探方向[J].石油实验地质,2004,26(1):23~27.
    [7]
    何发岐.塔里木盆地塔河油田油气勘探新技术[J].石油实验地质,2001,23(3):318~322.
    [8]
    张宝民.塔里木盆地寒武-奥陶系烃源岩特征及其发育的控制因素初探[A].见:王宜林编.第五届全国沉积学及岩相古地理学学术会议论文集[C].乌鲁木齐:新疆科技卫生出版社,1997.319~322.
    [9]
    梁狄刚.塔里木盆地九年油气勘探历程与回顾(续)[J].勘探家:石油与天然气,1999,4(2):53~56.
    [10]
    顾乔元,潘文庆.轮南地区奥陶系油气成藏特征[J].新疆石油地质,1999,20(3):210~212
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