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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2010  >  32(2): 108-114
Peng Shoutao, He Zhiliang, Ding Yong, Zhang Tao, Xia Dongling, Ji Shengzhen, Yun Jinbiao. CHARACTERISTICS AND MAJOR CONTROLLING FACTORS OF CARBONATES RESERVOIR IN THE MIDDLE ORDOVICIAN YIJIANFANG FORMATION, TUOFUTAI AREA, TAHE OILFIELD[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(2): 108-114. doi: 10.11781/sysydz201002108
Citation: Peng Shoutao, He Zhiliang, Ding Yong, Zhang Tao, Xia Dongling, Ji Shengzhen, Yun Jinbiao. CHARACTERISTICS AND MAJOR CONTROLLING FACTORS OF CARBONATES RESERVOIR IN THE MIDDLE ORDOVICIAN YIJIANFANG FORMATION, TUOFUTAI AREA, TAHE OILFIELD[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(2): 108-114. doi: 10.11781/sysydz201002108
shu

CHARACTERISTICS AND MAJOR CONTROLLING FACTORS OF CARBONATES RESERVOIR IN THE MIDDLE ORDOVICIAN YIJIANFANG FORMATION, TUOFUTAI AREA, TAHE OILFIELD

doi: 10.11781/sysydz201002108
  • 1.

    Exploration & Production Research Institute, SINOPEC, Beijing 100083, China

  • 2. Research Institute of Exploration & Production, Northwest Company of SINOPEC, Urumqi 830011, China

  • Received Date: 2009-12-03
  • Rev Recd Date: 2010-03-04
  • Publish Date: 2010-04-28
    Abstract
  • Based on analysis of 30 wells data of logging,well logging,oil production test,geophysical,and rock core and rock thin-section observation,the results show dissolved pores and/or caves,factures are the main reservoir spaces with low matrix porosity in Middle Ordovician Yijianfang Formation,Tuofutai area of Tahe Oilfield.On the plane the reservoir types have the feature of "north-south zoning distribution,east-west heterogeneity".The karst reservoirs mainly formed in middle Caledonian and were controlled by such factors as paleo-geomorphology,faults or fractures,lithology and facies,etc.,showing distinct features of fault-controlled and strata-bound.Thus it is predicted that the areas of favorable reservoir rocks would be developed in the congruent sites of the high position of Caledonian paleo-geomorphology,concentration area of faults or fractures and high energy reef-flat facies,which are mainly distributed in the middle and northern part of Tuofutai area.

     

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    • References(26)
  • [1]
    祝贺,刘家铎,孟万斌,等.塔河油田托甫台地区中下奥陶统沉积相与储层特征分析[J].成都理工大学学报(自然科学版),2008,35(3):232-237.
    [2]
    陈强路,王恕一,钱一雄,等.塔里木盆地阿克库勒地区下奥陶统古岩溶及油气分布[J].沉积学报,2002,20(4):633-637.
    [3]
    杨宁,吕修祥,陈梅涛,等.塔里木盆地轮南、塔河油田碳酸盐岩储层特征研究:以沙107井和轮古40井为例[J].石油实验地质,2008,30(3):247-251.
    [4]
    闫相宾,张涛.塔河油田碳酸盐岩大型隐蔽油藏成藏机理探讨[J].地质论评,2004,50(4):370-376.
    [5]
    李国蓉.阿克库勒凸起奥陶系碳酸盐岩岩溶作用及成藏机制[R].乌鲁木齐:中国石油化工股份有限公司西北分公司,2004.
    [6]
    艾合买提江·阿不都热和曼,钟建华,李阳,等.碳酸盐岩裂缝与岩溶作用研究[J].地质论评,2008,54(4):485-493.
    [7]
    俞仁连,傅恒.构造运动对塔河油田奥陶系碳酸盐岩的影响[J].天然气勘探与开发,2006,29(2):1-5.
    [8]
    吕海涛,张卫彪,张达景,等.塔里木盆地塔河油田奥陶系油气成藏演化过程研究[J].石油实验地质,2008,30(6):547-551,556.
    [9]
    蔡忠贤,刘永立,段金宝.岩溶流域的水系变迁:以塔河油田6区西北部奥陶系古岩溶为例[J].中国岩溶,2009,28(1):30-35.
    [10]
    孟万斌,刘家铎,何建军,等.塔河托甫台地区一间房组储层特征与地震预测[C].油气藏地质及开发工程国家重点实验室第五次国际学术研讨会(上册).成都:[出版者不详],2009:212-217.
    [11]
    康玉柱.中国塔里木盆地石油地质特征及资源评价[M].北京:地质出版社,1996:1-15.
    [12]
    金之钧,张一伟,陈书平.塔里木盆地构造-沉积波动过程[J].中国科学D辑:地球科学,2005,48(6):530-549.
    [13]
    赵锡奎,何建军,张小兵,等.阿克库勒凸起构造演化与古构造研究[R].乌鲁木齐:中国石化西北油田分公司勘探开发研究院,2009.
    [14]
    朱光有,张水昌,王欢欢,等.塔里木盆地北部深层风化壳储层的形成与分布[J].岩石学报,2009,25(10):2384-2398.
    [15]
    闫相宾,韩振华,李永宏.塔河油田奥陶系油藏的储集特征和成因机理探讨[J].地质论评,2002,48(6):619-626.
    [16]
    李翎,魏斌,贺铎华.塔河油田奥陶系碳酸盐岩储层的测井解释[J].石油与天然气地质,2002,23(1):49-55.
    [17]
    CHARLES K.Karst-controlled reservoir heterogeneity in Ellenburger Group carbonates of west Texas[J].AAPG Bulletin,1988,72(10):1160-1183.
    [18]
    陈景山,李忠,王振宇,等.塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布[J].沉积学报,2007,25(6):858-868.
    [19]
    吕修祥,杨宁,周新源,等.塔里木盆地断裂活动对奥陶系碳酸盐岩储层的影响[J].中国科学D辑:地球科学,2008,38(增刊Ⅰ):48-54.
    [20]
    俞仁连.塔里木盆地塔河油田加里东期古岩溶特征及其意义[J].石油实验地质,2005,27(5):468-472.
    [21]
    刘春燕,吴茂炳,巩固.塔里木盆地北部塔河油田奥陶系岩溶作用及其油气地质意义[J].地质通报,2006,25(9/10):1128-1134.
    [22]
    刘存革,李国蓉,朱传玲,等.塔河油田中下奥陶统岩溶缝洞方解石碳、氧、锶同位素地球化学特征[J].地球科学:中国地质大学学报,2008,33(3):377-386.
    [23]
    刘文,李永宏,张涛,等.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.
    [24]
    孙龙德.塔里木含油气盆地沉积学研究进展[J].沉积学报,2004,22(3):408-416.
    [25]
    丁文龙,高峰,陆文凯,等.塔河油田西南部上奥陶统覆盖区中下奥陶统储层构造控制作用与评价[R].乌鲁木齐:中国石化西北分公司勘探开发研究院,2007.
    [26]
    龚福华,刘小平.塔里木盆地轮古西地区断裂对奥陶系古岩溶的控制作用[J].中国岩溶,2003,22(4):313-317.
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