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塔里木盆地中央隆起区恰尔巴克组与一间房组分布及意义

蔡习尧 马宇驰 陈跃 钱一雄 尤东华

蔡习尧, 马宇驰, 陈跃, 钱一雄, 尤东华. 塔里木盆地中央隆起区恰尔巴克组与一间房组分布及意义[J]. 石油实验地质, 2015, 37(5): 591-598. doi: 10.11781/sysydz201505591
引用本文: 蔡习尧, 马宇驰, 陈跃, 钱一雄, 尤东华. 塔里木盆地中央隆起区恰尔巴克组与一间房组分布及意义[J]. 石油实验地质, 2015, 37(5): 591-598. doi: 10.11781/sysydz201505591
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

塔里木盆地中央隆起区恰尔巴克组与一间房组分布及意义

doi: 10.11781/sysydz201505591
基金项目: 国家油气重大专项(2011ZX05005-004-003-002)和国家重点基础研究发展计划(973计划)(06-2012CB214806)资助。
详细信息
    作者简介:

    蔡习尧(1963—),男,高级工程师,从事地层古生物与石油勘探研究。E-mail:caixy.syky@sinopec.com。

  • 中图分类号: TE121.3+4

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

  • 摘要: 塔里木盆地中央隆起区共有10口探井钻遇了上奥陶统恰尔巴克组及中奥陶统一间房组,分属上奥陶统良里塔格组/恰尔巴克组/一间房组/鹰山组与却尔却克组/恰尔巴克组/一间房组/鹰山组2种不同的地层层序。恰尔巴克组为紫红、褐、灰色泥晶灰岩、泥灰岩及灰质泥岩,厚度17~25 m,属于斜坡相沉积,底部产Pygodus anserinus化石带。一间房组为灰色泥晶砂屑灰岩、颗粒灰岩及生屑灰岩,厚度80~120 m,属开阔台地—台地边缘相沉积,顶部产Pygodus serrus化石带。恰尔巴克组与一间房组分布在隆起边缘的低洼部位及隆起往坳陷的过渡区,在隆起的主体上分别为沉积缺失与剥蚀缺失。中央隆起区奥陶系分为隆起区、过渡区(A、B)与坳陷区,过渡区的西边界至少西推了100 km,中晚奥陶世区内为开阔台地—台缘—斜坡相沉积,不发育"萨尔干组"型的烃源岩,过渡区具备2套良好的储盖组合,为有利的油气勘探区。

     

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  • 收稿日期:  2014-08-06
  • 修回日期:  2015-08-11
  • 刊出日期:  2015-09-28

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