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    石臼坨凸起西南陡坡带扇三角洲锆石定年与源汇示踪

    赵梦 徐长贵 杜晓峰 王清斌

    赵梦, 徐长贵, 杜晓峰, 王清斌, 2017. 石臼坨凸起西南陡坡带扇三角洲锆石定年与源汇示踪. 地球科学, 42(11): 1984-1993. doi: 10.3799/dqkx.2017.126
    引用本文: 赵梦, 徐长贵, 杜晓峰, 王清斌, 2017. 石臼坨凸起西南陡坡带扇三角洲锆石定年与源汇示踪. 地球科学, 42(11): 1984-1993. doi: 10.3799/dqkx.2017.126
    Zhao Meng, Xu Changgui, Du Xiaofeng, Wang Qingbin, 2017. Detrital Zircon U-Pb Geochronology and Provenance Tracing of the Fan Deltas along the Southwestern Slope of the Shijiutuo Uplift. Earth Science, 42(11): 1984-1993. doi: 10.3799/dqkx.2017.126
    Citation: Zhao Meng, Xu Changgui, Du Xiaofeng, Wang Qingbin, 2017. Detrital Zircon U-Pb Geochronology and Provenance Tracing of the Fan Deltas along the Southwestern Slope of the Shijiutuo Uplift. Earth Science, 42(11): 1984-1993. doi: 10.3799/dqkx.2017.126

    石臼坨凸起西南陡坡带扇三角洲锆石定年与源汇示踪

    doi: 10.3799/dqkx.2017.126
    基金项目: 

    国家"十三五"科技重大专项 2016ZX05024003

    详细信息
      作者简介:

      赵梦(1987-), 女, 勘探地质工程师, 博士, 主要从事沉积学、地质学研究

    • 中图分类号: P736.21

    Detrital Zircon U-Pb Geochronology and Provenance Tracing of the Fan Deltas along the Southwestern Slope of the Shijiutuo Uplift

    • 摘要: 为了示踪渤海湾盆地石臼坨凸起西南陡坡带扇三角洲源汇体系,对其东三段层序(Ed3)的6个砂岩样品进行碎屑锆石U-Pb定年分析.西部扇体(C6-4-4井)富含白垩纪(K)锆石并具有110 Ma峰值,母岩以白垩系义县组火成岩为主;中部(C6-4-3、C6-4-6D井)、东部扇体(C6-4-5D)富含侏罗纪(J)锆石并具有152 Ma或168 Ma峰值,母岩以侏罗系蓝旗组火成岩为主,古生代(Pz)锆石则来自中生界碎屑岩.所有样品都含有太古代(Ar)、元古代(Pt)锆石,母岩为花岗岩基底.研究表明,除古生界碳酸盐岩外,源区的母岩地层均可通过碎屑锆石U-Pb年龄示踪,各扇体物源的差异性是由母岩地层倾向控制的,由于中生界向西北倾斜,白垩系主控西部扇体沉积,侏罗系则是中部、东部扇体的主要物源区.

       

    • 图  1  石臼坨凸起西部残余地层地质图及井位、地震剖面位置

      岩性修改自庞小军等(2016);沟谷修改自王启明等(2016)

      Fig.  1.  The geology map of the remaining strata on the western Shijiutuo uplift and the location of the wells and the seismic profiles

      图  2  各井位东三段岩性及取样位置示意

      红色星号为取样位置

      Fig.  2.  The Ed3 lithology of the wells and their sample depth

      图  3  曹妃甸6-4构造东三段砂岩碎屑锆石Th/U比值

      Fig.  3.  The Th/U ratio of the detrital zircons of the Ed3 sandstone, CFD6-4

      图  4  曹妃甸6-4构造东三段砂岩碎屑锆石U-Pb年龄含量分布

      Fig.  4.  The U-Pb age composition distribution of the detrital zircons of the Ed3 sandstone, CFD6-4

      图  5  曹妃甸6-4构造东三段砂岩碎屑锆石U-Pb年龄谱图

      n为年龄点个数

      Fig.  5.  The U-Pb age spectra of the detrital zircons of the Ed3 sandstone, CFD6-4

      图  6  曹妃甸6-4构造过井地震剖面与残余侏罗系

      剖面位置及图例见图 1

      Fig.  6.  The cross-well seismic profiles, CFD6-4 and the recovered Jurassic

      表  1  曹妃甸6-4构造东三段砂岩碎屑锆石U-Pb年龄含量统计(%)

      Table  1.   The U-Pb age composition of the detrital zircons of the Ed3 sandstone, CFD6-4

      井名 年龄(Ma) <140 <208 <250 <290 <362 <409 <439 <510 <570 <1 000 <1 800 <2 500 <2 500 Mz Pz2 Pz1
      点数 K J T P C D S O Pt3 Pt2 Pt1 Ar
      C6-4-4 45 42.2 4.4 8.9 0.0 2.2 0.0 0.0 0.0 0.0 0.0 4.4 22.2 15.6 55.6 2.2 0.0
      C6-4-3 71 4.2 19.7 4.2 9.9 7.0 1.4 0.0 0.0 0.0 1.4 11.3 23.9 16.9 28.2 18.3 0.0
      C6-4-6D 112 3.6 13.4 2.7 8.0 8.9 1.8 1.8 0.0 0.0 1.8 11.6 32.1 14.3 19.6 18.8 1.8
      C6-4-5D 63 3.2 25.4 11.1 4.8 6.3 3.2 1.6 1.6 0.0 0.0 9.5 17.5 15.9 39.7 14.3 3.2
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