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    丽水-椒江凹陷西斜坡明月峰组上段碎屑锆石物源

    付晓伟 朱伟林 陈春峰 钟锴 许长海

    付晓伟, 朱伟林, 陈春峰, 钟锴, 许长海, 2015. 丽水-椒江凹陷西斜坡明月峰组上段碎屑锆石物源. 地球科学, 40(12): 1987-2001. doi: 10.3799/dqkx.2015.178
    引用本文: 付晓伟, 朱伟林, 陈春峰, 钟锴, 许长海, 2015. 丽水-椒江凹陷西斜坡明月峰组上段碎屑锆石物源. 地球科学, 40(12): 1987-2001. doi: 10.3799/dqkx.2015.178
    Fu Xiaowei, Zhu Weilin, Chen Chunfeng, Zhong Kai, Xu Changhai, 2015. Detrital Zircon Provenance of Upper Mingyuefeng Formation in West Slope of Lishui-Jiaojiang Sag, the East China Sea. Earth Science, 40(12): 1987-2001. doi: 10.3799/dqkx.2015.178
    Citation: Fu Xiaowei, Zhu Weilin, Chen Chunfeng, Zhong Kai, Xu Changhai, 2015. Detrital Zircon Provenance of Upper Mingyuefeng Formation in West Slope of Lishui-Jiaojiang Sag, the East China Sea. Earth Science, 40(12): 1987-2001. doi: 10.3799/dqkx.2015.178

    丽水-椒江凹陷西斜坡明月峰组上段碎屑锆石物源

    doi: 10.3799/dqkx.2015.178
    基金项目: 

    国家科技重大专项 2011ZX05023-003

    详细信息
      作者简介:

      付晓伟(1986-),男,博士研究生,主要从事沉积及构造地质方面的研究.E-mail:shjzhfxw@163.com

    • 中图分类号: P618

    Detrital Zircon Provenance of Upper Mingyuefeng Formation in West Slope of Lishui-Jiaojiang Sag, the East China Sea

    • 摘要: 沉积物源对油气储层发育具有重要影响.为研究丽水-椒江凹陷西斜坡明月峰组上段物源的岩性组成及其分布特征,选取4口钻井4个砂岩样品进行碎屑锆石U-Pb定年,并对陆上潜在物源区岩层(体)的岩性和年龄进行统计分析.结果显示:(1)样品中碎屑锆石以岩浆锆石为主,主要的年龄区间为125~90 Ma、145~125 Ma及170~145 Ma,还有少量变质锆石,其年龄区间为235~210 Ma及2 087~1 653 Ma;(2)陆上潜在物源区中以火山岩占绝对优势(173~94 Ma),局部区域可能有较大规模白垩系永康群沉积岩,而变质岩(>210 Ma)和侵入岩(107.0~87.8 Ma)仅零星出露.综合分析认为:研究区东北部明月峰组上段的物源以永康群火山-沉积岩和九里坪组火山岩为主,含有少量晚白垩世侵入岩;西南部以九里坪组、西山头组火山岩及元古代区域变质岩为主,侏罗纪火山岩为辅,这一区域可能更有利于优质储层的发育.

       

    • 图  1  丽水-椒江凹陷及潜在物源区地质

      浙江省地质矿产局(1989)福建省地质矿产局(1985)修改;瓯江流域样品位置据Xu et al.(2007);侵入岩体年龄据邱检生等(2008, 2011)、李艳军等(2009, 2010)和He and Xu(2012)

      Fig.  1.  Geology of Lishui-Jiaojiang sag and potential source area

      图  2  丽水-椒江凹陷沉积地层综合柱状图(a)和浙东南地层区前新生代地层综合柱状图(b)

      图a据田兵等(2012)修改;图b岩性据张国全等(2012)浙江省地质矿产局(1989)

      Fig.  2.  Comprehensive stratigraphic column in Lishui-Jiaojiang sag (a) and comprehensive Pre-Cenozoic stratigraphic column of southeastern Zhejiang stratigraphic region (b)

      图  3  碎屑锆石样品锆石U-Pb年龄协和图

      Fig.  3.  Concordia plot for analyzed detrital zircon samples

      图  4  丽水-椒江凹陷碎屑锆石典型CL图像特征

      Fig.  4.  Cathodoluminscence (CL) image of typical detrital zircons from Lishui-Jiaojiang sag

      图  5  定年样品的碎屑锆石Th/U值

      Fig.  5.  Th/U ratio of zircons analyzed in this study

      图  6  丽水凹陷明月峰组碎屑锆石年龄谱(n为测试锆石颗粒数)

      Fig.  6.  Detrital-zircon age-spectra from Mingyuefeng Formation in Lishui sag

      图  7  浙闽沿海晚中生代火山岩锆石及瓯江流域碎屑锆石U-Pb年龄累积概率曲线

      瓯江流域数据据文献Xu et al.(2007);浙闽火山岩数据据文献余明刚等(2006)邢光福等(2008)Li et al.(2009)崔玉荣等(2010)Guo et al.(2012)Liu et al.(2012)Hu et al.(2012)段政等(2013)

      Fig.  7.  Cumulative probability curve of zircon U-Pb age of Oujiang River and late Mesozoic volcanic rocks around Fujian and Zhejiang coastal

      图  8  闽浙陆域前新生代不同岩层(体)锆石U-Pb年龄分布

      数据据赵磊(2012)Xu et al.(2007)胡艳华等(2011)向华等(2008)陈多福等(1998)Wan et al.(2007)Li et al.(2014)邱检生等(2008, 2011)、李艳军等(2009, 2010)、He and Xu(2012)Guo et al.(2012)

      Fig.  8.  The distribution of zircon U-Pb ages in the different Pre-Cenozoic strata(intrusive mass) of Fujian and Zhejiang region

      表  1  瓯江及飞云江-鳌江流域岩层(体)和岩性分布

      Table  1.   Rocks and its lithological distribution in Oujiang and Feiyunjiang-Aojiang River

      瓯江流域(18 168.75 km2) 飞云江-鳌江流域(6 630.00 km2)
      岩层(体) 面积(%) 沉积岩 面积(%) 沉积岩
      剖面(%) 权重比例(%) 剖面(%) 权重比例(%)
      永康群 方岩组 1.3 沉积岩为主 1.3 0
      馆头组 3.4 31.0~88.3 1.1~3.0 10.8 沉积岩 10.8
      朝川组 1.8 31.8~93.3 0.6~1.7 15.3 31.8~70.0 4.9~10.7
      磨石山群 九里坪组 5.1 极少 0 5.8 极少 0
      茶湾组 0.1 沉积岩为主 0.1 0.4 沉积岩为主 0.4
      西山头组 30.8 0~3.6 0~1.1 28.1 0.7~19.0 0.02~5.30
      高坞组 24.8 0~7.8 0~1.9 10.4 极少 0
      大爽组 12.7 极少~39.5 0~5 0 0
      变质岩 5.2 0 0 0
      侵入岩 9.1 0 0 12.3
      第四纪 4.5 28.3
      其他 1.1 1.1 0.8 0.8
      总计(第四纪除外) 火山岩+变质岩+侵入岩79.8%~91.7% 沉积岩+其他9.3%~20.2%
      注:沉积岩权重比例(%)=流域内岩层面积比(%)×剖面中沉积岩厚度比例(%),其他为长林组(沉积岩为主)和祝村组(无锆石U-Pb定年数据),剖面沉积岩比例据浙江省地质矿产局(1989)张国全等(2012).
      下载: 导出CSV
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