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    华北克拉通胶北地体蓬莱群辅子夼组碎屑锆石U-Pb定年及其地质意义

    王宏宇 王义龙 刘平华 周万蓬 张宇佳 张传恒

    王宏宇, 王义龙, 刘平华, 周万蓬, 张宇佳, 张传恒, 2021. 华北克拉通胶北地体蓬莱群辅子夼组碎屑锆石U-Pb定年及其地质意义. 地球科学, 46(9): 3074-3090. doi: 10.3799/dqkx.2021.061
    引用本文: 王宏宇, 王义龙, 刘平华, 周万蓬, 张宇佳, 张传恒, 2021. 华北克拉通胶北地体蓬莱群辅子夼组碎屑锆石U-Pb定年及其地质意义. 地球科学, 46(9): 3074-3090. doi: 10.3799/dqkx.2021.061
    Wang Hongyu, Wang Yilong, Liu Pinghua, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Detrital Zircon U-Pb Dating of the Fuzikuang Formation, Penglai Group in Jiaobei Terrane, North China Craton and Its Geological Significance. Earth Science, 46(9): 3074-3090. doi: 10.3799/dqkx.2021.061
    Citation: Wang Hongyu, Wang Yilong, Liu Pinghua, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Detrital Zircon U-Pb Dating of the Fuzikuang Formation, Penglai Group in Jiaobei Terrane, North China Craton and Its Geological Significance. Earth Science, 46(9): 3074-3090. doi: 10.3799/dqkx.2021.061

    华北克拉通胶北地体蓬莱群辅子夼组碎屑锆石U-Pb定年及其地质意义

    doi: 10.3799/dqkx.2021.061
    基金项目: 

    国家自然科学基金项目 41672191

    国家自然科学基金项目 41972205

    中国地质调查局地质大调查二级项目 DD20190003

    中国地质调查局地质大调查二级项目 DD20190370

    详细信息
      作者简介:

      王宏宇(1996-), 男, 硕士研究生, 主要从事地层学研究, ORCID: 0000-0003-0640-3292.E-mail: why96910@126.com

      通讯作者:

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

    • 中图分类号: P581

    Detrital Zircon U-Pb Dating of the Fuzikuang Formation, Penglai Group in Jiaobei Terrane, North China Craton and Its Geological Significance

    • 摘要: 蓬莱群是胶北地区最主要的晚前寒武纪沉积盖层,对研究华北克拉通东南缘晚前寒武纪演化有重要意义.为确认蓬莱群沉积时代与物源特征,本次研究选取栖霞地区蓬莱群辅子夼组中上部的长石石英岩为研究对象,对锆石CL图像、U-Pb年龄以及稀土元素组成开展研究,发现碎屑锆石主要为岩浆锆石,年龄峰值主要集中在1 100、1 200 Ma以及1 600 Ma,缺乏年龄大于1.8 Ga的锆石;其中,最年轻碎屑锆石年龄为1 094±39 Ma,结合前人资料,蓬莱群辅子夼组沉积时代被限定在新元古代初期;不同地区的蓬莱群在辅子夼组中部以上物源区是统一的,在辅子夼组下部沉积时期物源发生变化.在区域上,蓬莱群物源特点与朝鲜祥原超群、以及我国辽东细河群、鲁南土门群、徐淮地区淮南群、豫西地区栾川群等华北东缘、南缘新元古代沉积盆地物源相似,物源主要来自华北克拉通以外的古陆.结合古地磁、中—新元古代岩墙分布等资料,推测发育格林威尔期造山带的克拉通如Laurentia-Siberia-Baltica或Sao Fransico-Congo克拉通与华北克拉通南缘拼合,提供物源.

       

    • 图  1  胶北地区地质简图

      修改自Zhao et al.(2012)

      Fig.  1.  Simplified geology map of Jiaobei terrane

      图  2  研究区地质简图

      1.太古宙英云闪长质‒花岗闪长质片麻岩;2.太古宙变基性岩;3.古元古代变基性岩;4.粉子山群;5.蓬莱群豹山口组6.蓬莱群辅子夼组;7.蓬莱群南庄组;8.蓬莱群香夼组;9.白垩系;10.白垩纪侵入岩;11.第四系;12.韧性剪切带;13.断层

      Fig.  2.  Geological sketch of the study area

      图  3  蓬莱群地层柱状图

      Fig.  3.  Stratigraphic column of the Penglai Group

      图  4  蓬莱群野外照片

      a.辅子夼组中段小型M型褶皱及其中差异风化现象;b.辅子夼组细粒石英岩夹纹层状板岩(采样位置);c. 辅子夼组上部石英岩中斜层理;e.豹山口组绢云绿泥板岩

      Fig.  4.  Field photographs of the Penglai Group

      图  5  样品19LR306-1镜下照片

      图a、c为单偏光;图b、d为正交偏光;Qz.石英;Pl.斜长石;Ser.绢云母

      Fig.  5.  Microphotographs of sample 19LR306-1

      图  6  代表性碎屑锆石CL图像及其207Pb/206Pb年龄

      Fig.  6.  Cathodoluminescence images and 207Pb/206Pb ages of zircons

      图  7  各组锆石谐和图(a, c, e)和球粒陨石标准化后稀土元素配分模式图(d, f)和锆石年龄概率密度图(b)

      球粒陨石稀土数据据Sun and McDonough(1989)

      Fig.  7.  Concordia diagrams (a, c, e) and CI-normalized REE patterns (d, f) and probility density plot (b) of feldspar quartzite

      图  8  华北克拉通南缘新元古代早期形态重建(a),及各地区该期地层碎屑锆石年龄对比(b)

      图a修改自Zhang et al.(2016)Kim et al.(2019);图b中绿色区为共同具有的1 200、1 600 Ma峰值,红色区为不同峰值,数据引自Li et al.(2007)Zhou et al.(2008)高林志等(2010)初航等(2011)Hu et al.(2012)Yang et al.(2012)朴贤旭等(2016a, 2016b)、田德欣等(2018)Kim et al.(2019)周光照等(2019)李振生等(2020)以及本文

      Fig.  8.  Reconstruction of the south margin of the North China Craton in early Neoproterozoic (a), and comparison of detrital zircon ages of strata this period in different areas (b)

      图  9  华北克拉通南缘地层碎屑锆石年龄与Laurentia-Baltica-Siberia和Sao Fransico以及North Australia克拉通对比

      图中灰色框代表~1 200、1 600 Ma年龄峰值;数据引自Babinski et al.(2012)Souza et al.(2019)Rodrigues et al.(2012)Khudoley et al.(2015)Aleinikoff et al.(2013)Bingen et al.(2011)Agyei-Dwarko et al.(2012)Zhang et al.(2017, 2018)、Yang et al.(2018)Peng et al.(2011)de Castro et al.(2019)Ernst et al.(2016)以及图 8所引用数据

      Fig.  9.  Detrital zircon ages of Neoproterozoic strata in the southern margin of the North China Craton comparison with Laurentia-Baltica-Siberia Craton、Sao Fransico craton and North Australia Craton

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