Advanced Search
Volume 37 Issue 5
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2015  >  37(5): 591-598
Cai Xiyao, Ma Yuchi, Chen Yue, Qian Yixiong, You Donghua. Distribution and significance of the Ordovician Qrebake and Yijianfang formations in the Central Uplift of the Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2015, 37(5): 591-598. doi: 10.11781/sysydz201505591
Citation: Cai Xiyao, Ma Yuchi, Chen Yue, Qian Yixiong, You Donghua. Distribution and significance of the Ordovician Qrebake and Yijianfang formations in the Central Uplift of the Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2015, 37(5): 591-598. doi: 10.11781/sysydz201505591
shu

Distribution and significance of the Ordovician Qrebake and Yijianfang formations in the Central Uplift of the Tarim Basin

doi: 10.11781/sysydz201505591
  • 1.

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

  • 2. College of Geosciences, China University of Petroleum, Beijing 102249, China

  • 3. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • Received Date: 2014-08-06
  • Rev Recd Date: 2015-08-11
  • Publish Date: 2015-09-28
    Abstract
  • The Qrebake Formation of the Upper Ordovician and the Yijianfang Formation of the Middle Ordovician have been intersected in ten wells in the Central Uplift of the Tarim Basin.They belong to two stratigraphic sequences: the Lianglitage/Qrebake/Yijianfang/Yingshan formations, and the Queerqueke/Qrebake/Yijianfang/Yingshan formations.The Qrebake Formation is composed of purplish red, brown and grey micritic limestones, marls and calcareous mudstones representative of slope facies.This formation is about 17-25 m thick, and has a Pygodus anserinus zone at the bottom.The Yijianfang Formation is composed of grey micritic sand-clastic limestones, grained limestones and bioclastic limestones representive of open platform and platform margin facies.This formation is about 80-120 m thick, and has a Pygodus serrus fossil zone at the top.The Qrebake and Yijianfang formations are mainly distributed in the lower parts of the uplift edge and the transition area from the uplift to the depression, while a sedimentary gap for the two formations is observed in the Central Uplift.The Ordovician of the Central Uplift is divided into the uplift zone, the transition zone (A, B), and the depression zone.The western boundary of the transition zone should be at least 100 km to the west compared to previous studies.During the Middle and Late Ordovician, the study area was an open platform to platform margin and slope facies, and developed no hydrocarbon source rocks of the "Salgan" type.Two sets of favorable reservoir and cap assemblages have been discovered in the transition zone, showing a good potential for hydrocarbon exploration.

     

    • FullText(HTML)
  • loading
    • References(21)
  • [1]
    何治亮,陈强路,钱一雄,等.塔里木盆地中央隆起区油气勘探方向[J].石油与天然气地质,2006,27(6):769-778.He Zhiliang,Chen Qianglu,Qian Yixiong,et al.Hydrocarbon exploration targets in central uplift area of Tarim basin[J].Oil & Gas Geology,2006,27(6):769-778.
    [2]
    何登发,周新源,张朝军,等.塔里木地区奥陶纪原型盆地类型及其演化[J].科学通报,2007,52(增刊I):126-135.He Dengfa,Zhou Xinyuan,Zhang Chaojun,et al.Tectonic types and evolution of Ordovician proto-type basins in the Tarim region[J].Chinese Science Bulletin,2007,52(SI):164-177.
    [3]
    贾承造,姚慧君,魏国齐,等.塔里木盆地板块构造演化和主要地质构造单元地质构造特征[C]//童晓光,梁狄刚.塔里木盆地油气勘探论文集.乌鲁木齐:新疆科技卫生出版社,1992:207-225.Jia Chengzao,Yao Huijun,Wei Guoqi,et al.Tectonic evolution and major tectonic units features of the Tarim Block[C]//Tong Xiaoguang, Liang Digang.Proceedings of the Oil and Gas Exploration in the Tarim Basin.Urumqi:Xinjiang Press of Science,Technology and Hygiene, 1992:207-225.
    [4]
    倪寓南,耿良玉,王志浩,等.奥陶系[M]//周志毅.塔里木盆地各纪地层.北京:科学出版社,2001:39-80.Ni Yu'nan,Geng Liangyu,Wang Zhihao,et al.Ordovician[M]//Zhou Zhiyi.Stratigraphy of the Tarim Basin.Beijing:Science Press, 2001:39-80.
    [5]
    贾承造,张师本,吴绍祖,等.塔里木盆地及周边地层[M].北京:科学出版社,2004:320-333.Jia Chengzao,Zhang Shiben,Wu Shaozu,et al.Stratigraphy of the Tarim Basin and adjacent areas[M].Beijing:Science Press, 2004:320-333.
    [6]
    杨海军,李勇,刘胜,等.塔中地区中、上奥陶统划分对比的主要认识[J].新疆石油地质,2000,21(3):208-212.Yang Haijun,Li Yong,Liu Sheng,et al.Classification and correlation of middle-upper Ordovician in Tazhong area and its key understanding[J].Xinjiang Petroleum Geology,2000,21(3):208-212.
    [7]
    黄智斌,邓胜徽,杜品德,等.塔里木盆地奥陶纪地层研究新进展[C]//周新源.塔里木会战20周年论文集.北京:石油工业出版社,2009:172-186.Huang Zhibin,Deng Shenghui,Du Pinde,et al.New advances in stratigraphic study on Ordovician in Tarim Basin[C]//Zhou Xinyuan.Paper Collection for the 20 Years Anniversary of Tarim Petroleum Meeting Campaign.Beijing:Petroleum Industry Press,2009:172-186.
    [8]
    蔡习尧,李越.新疆塔中南坡奥陶系的地层缺失和沉积相变[J].地层学杂志,2008,32(4):353-362.Cai Xiyao,Li Yue.Ordovician lithofacies and stratigraphic lacunae in the Southern part of the central Tarim,Xinjiang[J].Journal of Stratigraphy,2008,32(4):353-362.
    [9]
    董宝清,杜品德,刘兴礼,等.塔中88井奥陶系吐木休克组的发现及地层划分[J].新疆石油地质,2008,29(5):599-602.Dong Baoqing,Du Pinde,Liu Xingli,et al.Discovery of Tumu-xiuke formation of Upper Ordovician in Tazhong-88 well with stratigraphic division[J].Xinjiang Petroleum Geology,2008,29(5):599-602.
    [10]
    蔡习尧,钱一雄,陈强路,等.塔里木盆地古隆1井奥陶系恰尔巴克组与一间房组的发现及意义[J].石油实验地质,2011,33(4):348-352.Cai Xiyao,Qian Yixiong,Chen Qianglu,et al.Discovery and signification of Qrebake and Yijianfang Formations of Ordovician in well GL1,Tarim Basin[J].Petroleum Geology & Experiment,2011,33(4):348-352.
    [11]
    赵宗举,李宇平,吴兴宁,等.塔里木盆地塔中地区奥陶系特大型岩性油气藏成藏条件及勘探潜力[J].中国石油勘探,2004,9(5):12-20.Zhao Zongju,Li Yuping,Wu Xingning,et al.Conditions for migration and accumulation of giant Ordovician lithologic oil and gas reservoirs in Tazhong Region and exploration potential[J].China Petroleum Exploration,2004,9(5):12-20.
    [12]
    于炳松,陈建强,林畅松.塔里木盆地奥陶系层序地层格架及其对碳酸盐岩储集体发育的控制[J].石油与天然气地质,2005,26(3):305-309,316.Yu Bingsong,Chen Jianqiang,Lin Changsong.Sequence stratigraphic framework and its control on development of Ordovician carbonate reservoir in Tarim Basin[J].Oil & Gas Geology,2005,26(3):305-309,316.
    [13]
    赵宗举,潘文庆,张丽娟,等.塔里木盆地奥陶系层序地层格架[J].大地构造与成矿学,2009,33(1):175-188.Zhao Zongju,Pan Wenqing,Zhang Lijuan,et al.Sequence Stratigraphy in the Ordovician in the Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):175-188.
    [14]
    张师本,黄智斌,朱怀城,等.塔里木盆地覆盖区显生宙地层[M].北京:石油工业出版社,2004:1-300.Zhang Shiben,Huang Zhibin,Zhu Huaicheng,et al.Phanerozoic strata of Bestrow area in Tarim Basin[M].Beijing:Petroleum Industry Press,2004:1-300.
    [15]
    赵治信,张桂芝,肖继南.新疆古生代地层及牙形石[M].北京:石油工业出版社,2000:1-340.Zhao Zhixin,Zhang Guizhi,Xiao Jinan.Paleazoic stratigraphy and conodont in Xinjiang[M].Beijing:Petroleum Industry Press,2000:1-340.
    [16]
    熊剑飞,武涛,叶徳胜.新疆巴楚中—晚奥陶世牙形刺研究的新进展[J].古生物学报,2006,45(3):359-373.Xiong Jianfei,Wu Tao,Ye Desheng.New advances on the study of Middle-Late Ordovician Conodonts in Bachu, Xinjiang[J].Acta Palaeontologica Sinica,2006,45(3):359-373.
    [17]
    赵宗举,赵治信,黄智斌.塔里木盆地奥陶系牙形石带及沉积层序[J].地层学杂志,2006,30(3):193-203.Zhao Zongju,Zhao Zhixin,Huang Zhibin.Ordovician conodont zones and sedimentary sequences of the Tarim Basin, Xinjiang, NW China[J].Journal of Stratigraphy,2006,30(3):193-203.
    [18]
    蔡习尧,祁玉平,钱一雄,等.塔里木盆地古隆1井中上奥陶统牙形石生物地层界线研究[J].地质科学,2011,46(2):466-474.Cai Xiyao,Qi Yuping,Qian Yixiong,et al.Research of the biostratigraphy boundary on the Middle and Upper Ordovician in Well GL1 of Tarim Basin[J].Chinese Journal of Geology,2011,46(2):466-474.
    [19]
    张师本,倪寓南,龚福华,等.塔里木盆地周缘地层考察指南[M].北京:石油工业出版社,2003:18-26.Zhang Shiben,Ni Yunan,Gong Fuhua,et al.A guide to the stratigraphic investigation on the periphery of the Tarim Basin[M].Beijing:Petroleum Industry Press,2003:18-26.
    [20]
    陈旭,张元动,李越,等.塔里木盆地及周缘奥陶系黑色岩系的生物地层学对比[J].中国科学: D辑:地球科学,2012,42(8):1173-1181.Chen Xu,Zhang Yuandong,Li Yue,et al.Biostratigraphic correlation of the Ordovician black shales in Tarim Basin and its peripheral regions[J].Science China:Series D:Earth Sciences, 2012,42(8):1173-1181.
    [21]
    高志勇,张水昌,李建军,等.塔里木盆地西部中上奥陶统萨尔干页岩与印干页岩的空间展布与沉积环境[J].古地理学报,2010,12(5):599-608.Gao Zhiyong,Zhang Shuichang,Li Jianjun,et al.Distribution and sedimentary environments of Salgan and Yingan shales of the Middle-Upper Ordovician in western Tarim Basin[J].Journal of Palaeogeography,2010,12(5):599-608.
    • 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 (1113) PDF downloads(1004) 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