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    南秦岭封子山岩体的年代学、地球化学、Hf同位素特征及其地质意义

    柏治安 时毓 刘希军 黄倩雯 覃康乐

    柏治安, 时毓, 刘希军, 黄倩雯, 覃康乐, 2019. 南秦岭封子山岩体的年代学、地球化学、Hf同位素特征及其地质意义. 地球科学, 44(4): 1186-1201. doi: 10.3799/dqkx.2018.586
    引用本文: 柏治安, 时毓, 刘希军, 黄倩雯, 覃康乐, 2019. 南秦岭封子山岩体的年代学、地球化学、Hf同位素特征及其地质意义. 地球科学, 44(4): 1186-1201. doi: 10.3799/dqkx.2018.586
    Bai Zhi'an, Shi Yu, Liu Xijun, Huang Qianwen, Qin Kangle, 2019. Geochronology, Geochemistry and Hf Isotopes of Fengzishan Pluton in South Qinling and Its Geological Significance. Earth Science, 44(4): 1186-1201. doi: 10.3799/dqkx.2018.586
    Citation: Bai Zhi'an, Shi Yu, Liu Xijun, Huang Qianwen, Qin Kangle, 2019. Geochronology, Geochemistry and Hf Isotopes of Fengzishan Pluton in South Qinling and Its Geological Significance. Earth Science, 44(4): 1186-1201. doi: 10.3799/dqkx.2018.586

    南秦岭封子山岩体的年代学、地球化学、Hf同位素特征及其地质意义

    doi: 10.3799/dqkx.2018.586
    基金项目: 

    广西自然科学基金项目 2016GXNSFAA380001

    内生金属矿床成矿机制研究国家重点实验室(南京大学)开放基金项目 21-16-04

    广西自然科学基金项目 2017GXNSFBA198167

    国家自然科学基金项目 41562005

    广西"八桂学者"团队项目 2013,有色金属成矿理论与勘查技术

    国家自然科学基金项目 41302155

    详细信息
      作者简介:

      柏治安(1993-), 男, 硕士研究生, 主要从事岩石学研究

      通讯作者:

      时毓

    • 中图分类号: P597

    Geochronology, Geochemistry and Hf Isotopes of Fengzishan Pluton in South Qinling and Its Geological Significance

    • 摘要: 对南秦岭封子山岩体进行了锆石U-Pb年代学、岩石地球化学以及Hf同位素的研究,以确定其形成时代、岩体成因及形成时的构造环境.LA-ICP-MS锆石U-Pb定年测试结果表明,该岩体形成于新元古代晚期(716~710 Ma).锆石Hf同位素分析显示εHft)为-3.16~1.17,二阶段模式年龄(TDM2)为1.84~1.52 Ga.地球化学特征显示封子山岩体具高硅(62.92%~73.57%)、高钠(3.33%~4.22%),富集轻稀土元素,富集K、Rb、Ba、Th、U等大离子亲石元素,亏损Nb、Ta、Ti、P等高场强元素的特征,Eu显示弱负异常(δEu=0.79~0.95),为准铝质-弱过铝质中钾钙碱性Ⅰ型花岗岩.结果表明,封子山岩体主要来源于陡岭群片麻岩的部分熔融.封子山岩体形成于裂谷扩张与小洋盆间杂并存的构造环境,是洋壳向陆壳俯冲作用的产物,可能是Rodinia超大陆聚合与裂解事件在该地区作用的响应.

       

    • 图  1  东秦岭西峡地区地质简图(a)和陡岭群地质简图(b)

      图a据杨斌虎等(2011);图b据李淼(2003)

      Fig.  1.  Simplified geological map in the Xixia area of Eastern Qinling (a) and simplified geological map of the Douling Group (b)

      图  2  封子山岩体显微图像

      Pl.斜长石;Kfs.钾长石;Qtz.石英;Hbl.普通角闪石

      Fig.  2.  Microphotographs of the Fengzishan pluton

      图  3  封子山岩体中代表性锆石颗粒CL图像

      实圈为锆石U-Pb年龄剥蚀点,虚圈为Hf同位素分析点,图中数字分别为U-Pb年龄测定值(Ma)和εHf(t)值

      Fig.  3.  CL images of zircons of the Fengzishan pluton

      图  4  封子山岩体中锆石的U-Pb谐和图

      Fig.  4.  Concordia plots for zircons of the Fengzishan pluton

      图  5  封子山岩体中锆石的(176Hf/177Hf)i-U-Pb年龄图

      Fig.  5.  Plot of (176Hf/177Hf)i vs.U-Pb ages for zircons of the Fengzishan pluton

      图  6  封子山花岗岩TAS图解

      Middlemost(1994);文献1数据来源于李淼(2003),文献2数据来源于Zhang et al.(2004),下同

      Fig.  6.  TAS classification diagram for granitoids of the Fengzishan pluton

      图  7  封子山花岗岩类SiO2-K2O图解(a)和A/CNK-A/NK图解(b)

      图a据Peccerillo and Taylor(1976); 图b据Pearce et al.(1984)

      Fig.  7.  SiO2-K2O diagram (a) and A/CNK-A/NK diagram (b) for the Fengzishan pluton

      图  8  稀土模式配分图(a)和微量元素蛛网图(b)

      封子山的数据来源为李淼(2003)Zhang et al.(2004);陡岭群的数据来源为赵子然等(1995)张寿广等(2004)Shi et al.(2013);球粒陨石和原始地幔标准化值引自Sun and McDonough(1989)

      Fig.  8.  REE patterns (a) and spider diagram(b)

      图  9  封子山花岗岩成因系列Na2O-K2O图解

      Fig.  9.  Na2O-K2O diagram for granitoids of the Fengzishan pluton

      图  10  Rb-(Y+Nb)判别图(a)和Nb-Y判别图(b)

      Pearce et al.(1984).Syn-COLG.同碰撞型花岗岩;VAG.火山弧型花岗岩;WPG.板内型花岗岩;ORG.洋脊型花岗岩

      Fig.  10.  Rb-(Y+Nb) diagram of the granite (a) and Nb-Y factor diagram of the granites (b)

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