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    胶莱盆地蛇窝泊地区白垩纪林寺山组沉积时代与物源特征:来自碎屑锆石U-Pb测年与稀土元素组成的新证据

    张连祥 刘平华 王义龙 周万蓬 张宇佳 张传恒

    张连祥, 刘平华, 王义龙, 周万蓬, 张宇佳, 张传恒, 2021. 胶莱盆地蛇窝泊地区白垩纪林寺山组沉积时代与物源特征:来自碎屑锆石U-Pb测年与稀土元素组成的新证据. 地球科学, 46(3): 1119-1132. doi: 10.3799/dqkx.2020.403
    引用本文: 张连祥, 刘平华, 王义龙, 周万蓬, 张宇佳, 张传恒, 2021. 胶莱盆地蛇窝泊地区白垩纪林寺山组沉积时代与物源特征:来自碎屑锆石U-Pb测年与稀土元素组成的新证据. 地球科学, 46(3): 1119-1132. doi: 10.3799/dqkx.2020.403
    Zhang Lianxiang, Liu Pinghua, Wang Yilong, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Depositional Timing and Provenance Characteristics of the Cretaceous insishan Formation in the Shewopo Area, Jiaolai Basin: New Evidence from Detrital Zircon U-Pb Dating and REE Composition. Earth Science, 46(3): 1119-1132. doi: 10.3799/dqkx.2020.403
    Citation: Zhang Lianxiang, Liu Pinghua, Wang Yilong, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Depositional Timing and Provenance Characteristics of the Cretaceous insishan Formation in the Shewopo Area, Jiaolai Basin: New Evidence from Detrital Zircon U-Pb Dating and REE Composition. Earth Science, 46(3): 1119-1132. doi: 10.3799/dqkx.2020.403

    胶莱盆地蛇窝泊地区白垩纪林寺山组沉积时代与物源特征:来自碎屑锆石U-Pb测年与稀土元素组成的新证据

    doi: 10.3799/dqkx.2020.403
    基金项目: 

    国家自然科学基金项目 41972205

    国家自然科学基金项目 41672191

    中国地质调查局二级项目 DD20190003

    中国地质调查局二级项目 DD20190037

    详细信息
      作者简介:

      张连祥(1987-), 男, 博士研究生, 古生物学与地层学专业. ORCID: 0000-0002-7938-7943. E-mail: geoffreyzhang1105@163.com

      通讯作者:

      刘平华, ORCID: 0000-0001-5913-8627. E-mail: lph1213@126.com

    • 中图分类号: P581

    Depositional Timing and Provenance Characteristics of the Cretaceous insishan Formation in the Shewopo Area, Jiaolai Basin: New Evidence from Detrital Zircon U-Pb Dating and REE Composition

    • 摘要: 林寺山组是胶莱盆地莱阳群底部重要的地层单元之一.准确限定其沉积时代与物源性质对于客观重建华北陆块东部晚中生代大地构造格局以及周缘造山带/前寒武纪变质基底晚中生代的折返过程具有重要的制约作用.以莱阳盆地蛇窝泊地区莱阳群林寺山组细砾岩为研究对象,对其开展了野外地质调查、岩相学观察、锆石U-Pb测年与锆石稀土元素分析等综合研究,并获得了如下初步认识.(1)林寺山组细砾岩中最小一组碎屑锆石加权平均年龄分别为129±1 Ma与127±5 Ma,结合区域上不整合于莱阳群之上青山群火山岩锆石谐和年龄为119±1 Ma,推测蛇窝泊地区林寺山组沉积时代介于127~119 Ma.(2)蛇窝泊地区林寺山组细砾岩的碎屑锆石年龄变化于2 858~126 Ma之间,并以新太古代晚期与白垩纪早期碎屑锆石为主.前古元古代的碎屑锆石主要来源于胶北前寒武纪变质岩,表明胶北太古宙-古元古代变质岩至少在白垩纪早期已折返至近地表.(3)160~120 Ma岩浆型碎屑锆石主要来源于胶东同时代的中酸性侵入体,暗示在白垩纪早期至少部分160~120 Ma中酸性侵入体已抬升至地表.(4)林寺山组发育少量的二叠纪(280 Ma)和印支期(213 Ma)变质锆石,表明胶东地区可能存在二叠纪约280 Ma区域变质-变形事件,同时暗示早白垩世苏鲁超高压变质岩已经折返到地表.

       

    • 图  1  胶北地体地质简图

      修改自刘平华等(2015)

      Fig.  1.  Simplified geology map of the Jiaobei terrane

      图  2  胶北蛇窝泊地区地质简图

      Fig.  2.  Simplified geological map of the Shewopo area, Jiaobei terrane

      图  3  莱阳群划分与岩石单元

      Fig.  3.  The stratigraphic subdivision and lithostratigraphic units of the Laiyang Group

      图  4  胶北蛇窝泊地区莱阳群林寺山组紫红色砾岩与含砾粗砂岩野外露头照片

      a. 莱阳群林寺山组紫红色细砾岩原始层理;b. 莱阳群林寺山组紫红色中砾岩露头近照;c. 莱阳群林寺山组紫红色细砾岩露头近照;d. 莱阳群林寺山组紫红色含砾粗砂岩露头近照

      Fig.  4.  Field photographs showing the outcrops of the conglomerates and pebble-bearing coarse-grade sandstones from the Linsishan Formation of the Laiyang Group in the Shewopo area, Jiaobei terrane

      图  5  胶北蛇窝泊地区莱阳群林寺山组细砾岩代表性显微照片

      a~d. 莱阳群林寺山组紫红色细砾岩主要矿物组合:石英+斜长石+微斜长石+黑云母;a、c. 单偏光,b、d. 正交偏光;矿物缩写:Mc. 微斜长石;Bt. 黑云母;Pl. 斜长石;Qz. 石英

      Fig.  5.  Representative photomicrographs of the fine-grained conglomerate from the Linsishan Formation of the Laiyang Group in the Shewopo area of the Jiaobei terrane

      图  6  胶北蛇窝泊地区莱阳群林寺山组细砾岩中锆石阴极发光图像与U-Pb年龄

      Fig.  6.  Cathodoluminescence images and U-Pb ages of zircons from the fine-grained conglomerate from the Linsishan Formation of the Laiyang Group in the Shewopo area of the Jiaobei terrane

      图  7  胶北蛇窝泊地区莱阳群林寺山组细砾岩中锆石年龄频率直方图(a, b),U-Pb年龄谐和图(c, e, g)与稀土元素配分模式(d, f, h)

      球粒陨石稀土元素数据据Sun and McDonough(1989)

      Fig.  7.  Histogram with frequency distribution diagram (a and b), U-Pb age concordia diagram (c, e and g), (b) and CI-normalized REE patterns (d, f and h) of zircons from the fine-grained conglomerate from the Linsishan Formation of the Laiyang Group in the Shewopo area of the Jiaobei terrane

      图  8  胶北蛇窝泊地区莱阳群林寺山组细砾岩中锆石U-Pb年龄谐和图(a, c, e)与稀土元素配分模式图(b, d, f)

      球粒陨石稀土元素数据据Sun and McDonough(1989)

      Fig.  8.  U-Pb age concordia diagram (a, c and e), and CI-normalized REE patterns (b, d and f) of zircons from the fine-grained conglomerate from the Linsishan Formation of the Laiyang Group in the Shewopo area of the Jiaobei terrane

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