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    川东北地区飞仙关组台缘带鲕滩分布规律

    刘建强 罗冰 谭秀成 江兴福 李宗银 乔琳 薛玖火 赵长城

    刘建强, 罗冰, 谭秀成, 江兴福, 李宗银, 乔琳, 薛玖火, 赵长城, 2012. 川东北地区飞仙关组台缘带鲕滩分布规律. 地球科学, 37(4): 805-814. doi: 10.3799/dqkx.2012.089
    引用本文: 刘建强, 罗冰, 谭秀成, 江兴福, 李宗银, 乔琳, 薛玖火, 赵长城, 2012. 川东北地区飞仙关组台缘带鲕滩分布规律. 地球科学, 37(4): 805-814. doi: 10.3799/dqkx.2012.089
    LIU Jian-qiang, LUO Bing, TAN Xiu-cheng, JIANG Xing-fu, LI Zong-yin, QIAO Lin, XUE Jiu-huo, ZHAO Chang-cheng, 2012. Distribution of Marginal-Platform Oolitic Shoal in Feixianguan Formation, Northeast Sichuan, China. Earth Science, 37(4): 805-814. doi: 10.3799/dqkx.2012.089
    Citation: LIU Jian-qiang, LUO Bing, TAN Xiu-cheng, JIANG Xing-fu, LI Zong-yin, QIAO Lin, XUE Jiu-huo, ZHAO Chang-cheng, 2012. Distribution of Marginal-Platform Oolitic Shoal in Feixianguan Formation, Northeast Sichuan, China. Earth Science, 37(4): 805-814. doi: 10.3799/dqkx.2012.089

    川东北地区飞仙关组台缘带鲕滩分布规律

    doi: 10.3799/dqkx.2012.089
    基金项目: 

    中国石油科技创新基金研究项目 2011D-5006-0105

    国家“973”项目 2012CB214803

    详细信息
      作者简介:

      刘建强(1986-),男,在读硕士研究生,储层地质学.E-mail: liujq86@163.com

      通讯作者:

      谭秀成,E-mail: tanxiucheng70@163.com

    • 中图分类号: P618

    Distribution of Marginal-Platform Oolitic Shoal in Feixianguan Formation, Northeast Sichuan, China

    • 摘要: 对四川盆地飞仙关组台缘带鲕滩分布规律的认识不清,极大地制约着该区鲕滩气藏的勘探开发成效.以四川东北部飞仙关组为例,分析台缘带鲕滩的发育特征, 探索其分布规律.研究发现区内飞仙关组鲕滩沿台地边缘呈NW向展布,并在NE、NW两组基底正断裂交叉处向台地内部呈指状延伸,其延伸方向与台地边缘近于垂直.讨论认为基底断裂同沉积活动形成的古地理格局、沉积古地貌与相对海平面的升降变化共同控制了该区飞仙关组台缘带鲕滩的纵、横分布规律.指出NW向基底断裂的同沉积张裂活动形成了台坳分异的沉积格局,控制了台缘带及台缘带鲕滩相带展布;NE向基底断裂的同沉积正断活动加剧了台地边缘带的沉积地貌分异,台缘带鲕滩发育于NE-SW向基底断裂“断隆”地貌高地,并向台地内部延展,形成“北西控带、北东修饰”的断控型台缘鲕滩指状窄相带分布规律.考虑相对海平面升降变化对鲕滩沉积厚度及沉积范围的叠加影响,总结了台缘鲕滩的分布模式.

       

    • 图  1  川东北地区构造位置(据童崇光,1992修改)(a)及飞仙关组地层剖面(b)

      岩石圈深大断裂:①龙门山,②城口,③七曜山;地壳深大断裂:(1)龙泉山,(2)华蓥山,(3)铜锣峡,(4)明月峡,(5)黄泥堂,(6)巫溪-铁溪,(7)广元-利川;图中黑色虚线框示研究区

      Fig.  1.  Tectonic location of study area (a) and stratigraphic section of Feixianguan Formation (b)

      图  2  飞仙关组台缘带鲕滩常见岩石类型

      a.罗家9井,1(17/46),飞仙关组,鲕粒白云岩,普通薄片,单偏光,×5;b.渡3井,4 325.88 m,飞一段,鲕粒白云岩,铸体薄片,单偏光,×5;c.坡1井,3 424.08 m,飞二段,细粉晶白云岩,铸体薄片,单偏光,×5;d.七里北1井,5 809.33 m,飞二段,鲕粒白云岩,岩心照片

      Fig.  2.  Pictures showing the common rock type of marginal-platform oolitic shoal in Feixianguan Formation

      图  3  飞仙关组台缘带鲕滩纵向沉积序列

      a.普光2井飞仙关组二段(T1f2);b.坡1井飞仙关组二段(T1f2)

      Fig.  3.  Longitudinal sedimentary sequence of marginal-platform oolitic shoal in Feixianguan Formation

      图  4  台缘带鲕滩横向迁移模式示意

      Fig.  4.  Lateral migration model of marginal-platform oolitic shoal in study area

      图  5  研究区飞一、飞二期沉积相平面展布

      Fig.  5.  The horizontal distribution of sedimentary facies in Feixianguan period, north Sichuan

      图  6  川东北地区飞仙关组台缘带鲕滩分布模式

      Fig.  6.  The distribution model of marginal-platform oolitic shoal, northeast Sichuan

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    出版历程
    • 收稿日期:  2012-02-07
    • 网络出版日期:  2021-10-13
    • 刊出日期:  2012-07-15

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