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塔里木盆地顺托果勒低隆起一间房组分布及地质意义

尚凯 吕海涛 曹自成 韩俊 龚伟 黄诚

尚凯, 吕海涛, 曹自成, 韩俊, 龚伟, 黄诚. 塔里木盆地顺托果勒低隆起一间房组分布及地质意义[J]. 石油实验地质, 2018, 40(3): 353-361. doi: 10.11781/sysydz201803353
引用本文: 尚凯, 吕海涛, 曹自成, 韩俊, 龚伟, 黄诚. 塔里木盆地顺托果勒低隆起一间房组分布及地质意义[J]. 石油实验地质, 2018, 40(3): 353-361. doi: 10.11781/sysydz201803353
SHANG Kai, LÜ Haitao, CAO Zicheng, HAN Jun, GONG Wei, HUANG Cheng. Distribution and significance of Middle Ordovician Yijianfang Formation in Shuntuoguole lower uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(3): 353-361. doi: 10.11781/sysydz201803353
Citation: SHANG Kai, LÜ Haitao, CAO Zicheng, HAN Jun, GONG Wei, HUANG Cheng. Distribution and significance of Middle Ordovician Yijianfang Formation in Shuntuoguole lower uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(3): 353-361. doi: 10.11781/sysydz201803353

塔里木盆地顺托果勒低隆起一间房组分布及地质意义

doi: 10.11781/sysydz201803353
基金项目: 国家科技重大专项“塔里木盆地重点地区海相碳酸盐岩层系油气富集规律与目标评价”(2017ZX05005002-001)和中国石化科研项目“塔里木寒武系—中下奥陶统储层发育模式研究”(P16112)资助。
详细信息
    作者简介:

    尚凯(1982-),男,硕士,工程师,从事石油地质综合研究。E-mail:kaige925@163.com。

  • 中图分类号: TE122.3

Distribution and significance of Middle Ordovician Yijianfang Formation in Shuntuoguole lower uplift, Tarim Basin

  • 摘要: 在塔里木盆地顺托果勒低隆起相关钻井中获得了中奥陶世达瑞威尔期牙形石化石,由老到新分别为Eoplacognathus suecicus、Pygodus anitaePygodus serrus组合,为该区主要目的层之一的一间房组划分对比提供了较为详细的标准生物化石依据。同时,综合碳同位素地层、岩电特征和地震等资料,讨论了一间房组地层发育特征。在此基础上,通过连井地层划分对比和地震层位解释追踪,厘定了一间房组的分布范围。研究认为,一间房组在顺托果勒低隆起广泛分布,厚度为140~220 m,SN1-ST1井区厚度最大,超过了200 m。研究区一间房组—恰尔巴克组之间为连续沉积,不存在剥蚀不整合面,不具备发育加里东中期古喀斯特的地质条件。

     

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  • 收稿日期:  2017-12-21
  • 修回日期:  2018-04-02
  • 刊出日期:  2018-05-28

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