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    西秦岭印支早期铁堂峡石英正长斑岩的地球化学特征及其地质意义

    赵东辉 平先权 郑建平 艾磊 邓昊

    赵东辉, 平先权, 郑建平, 艾磊, 邓昊, 2019. 西秦岭印支早期铁堂峡石英正长斑岩的地球化学特征及其地质意义. 地球科学, 44(12): 4203-4221. doi: 10.3799/dqkx.2019.225
    引用本文: 赵东辉, 平先权, 郑建平, 艾磊, 邓昊, 2019. 西秦岭印支早期铁堂峡石英正长斑岩的地球化学特征及其地质意义. 地球科学, 44(12): 4203-4221. doi: 10.3799/dqkx.2019.225
    Zhao Donghui, Ping Xianquan, Zheng Jianping, Ai Lei, Deng Hao, 2019. Geochemistry and Its Geological Significance of the Quartz Syenites in the Early Indosinian from the Tietang Gorge, West Qinling. Earth Science, 44(12): 4203-4221. doi: 10.3799/dqkx.2019.225
    Citation: Zhao Donghui, Ping Xianquan, Zheng Jianping, Ai Lei, Deng Hao, 2019. Geochemistry and Its Geological Significance of the Quartz Syenites in the Early Indosinian from the Tietang Gorge, West Qinling. Earth Science, 44(12): 4203-4221. doi: 10.3799/dqkx.2019.225

    西秦岭印支早期铁堂峡石英正长斑岩的地球化学特征及其地质意义

    doi: 10.3799/dqkx.2019.225
    基金项目: 

    国家自然科学基金项目 41503018

    国家自然科学基金项目 41873038

    国家重点研发计划“深地资源勘查开采”重点专项资助项目 2016YFC0600403

    中国地质大学中央高校基本科研业务费专项资金资助项目 CUGCJ1814

    中国地质大学中央高校基本科研业务费专项资金资助项目 1810491A29

    详细信息
      作者简介:

      赵东辉(1997-), 男, 矿物学、岩石学和矿床学专业

      通讯作者:

      平先权

    • 中图分类号: P581

    Geochemistry and Its Geological Significance of the Quartz Syenites in the Early Indosinian from the Tietang Gorge, West Qinling

    • 摘要: 西秦岭东部发育大量小规模中酸性脉岩,但对这些脉岩的研究相对缺乏.在详细的野外观察和岩相学研究的基础上,对西秦岭天水铁堂峡石英正长斑岩进行了地球化学、锆石U-Pb年代学和Lu-Hf同位素研究.石英正长斑岩的锆石U-Pb定年结果表明它们的形成时代为~250 Ma,属印支早期岩浆产物.地球化学研究显示它们属于弱过铝质的高钾钙碱性岩系列,高Mg#,以富集Ba、Sr、K,强烈亏损Nb、Ta,且Eu异常不明显为特征.这些特征与埃达克岩的性质相似.铁堂峡石英正长斑岩的锆石εHft)值介于-1.44~+3.17,一阶段Hf模式年龄(tDM1)在765~945 Ma之间.铁堂峡石英正长斑岩形成于阿尼玛卿洋北向俯冲的大陆边缘弧环境,是俯冲洋壳及大洋沉积物熔体与上覆地幔楔作用的产物,并在浅部岩浆房中经历了轻微的分离结晶作用.

       

    • 图  1  西秦岭印支期中酸性岩体分布简图

      冯益民等(2002, 2003)修改

      Fig.  1.  Simplified geological map showing the distribution of Indosinian magmatic rocks in the West Qinling orogen

      图  2  西秦岭天水铁堂峡岩脉分布简图

      底图据1:20万天水幅

      Fig.  2.  Schematic diagram of the quartz syenite veins in Tietang Gorge, West Qinling

      图  3  西秦岭铁堂峡脉岩野外及镜下特征

      a~c.石英正长斑岩脉野外露头;d~f.石英正长斑岩镜下特征;g.石英正长斑岩与围岩烘烤边镜下特征;h~i.花岗斑岩镜下特征;Hb.角闪石;Or.正长石;Pl.斜长石;Qtz.石英;Cal.方解石

      Fig.  3.  Field photographs and photomicrographs of the dykes in the Tietang Gorge, West Qinling

      图  4  西秦岭铁堂峡石英正长斑岩代表性锆石CL图像

      黑圈为锆石年龄分析点,白圈为锆石Hf分析点;当t>1 000 Ma时,锆石年龄用的是207Pb/206Pb年龄,反之用的是206Pb/238U年龄

      Fig.  4.  CL images of representative zircons from the quartz syenites in the Tietang Gorge, West Qinling

      图  5  西秦岭铁堂峡石英正长斑岩锆石U-Pb谐和图

      a.18-H所有锆石U-Pb年龄谐和图;b.18-H岩浆结晶锆石年龄图;c.18-MO所有锆石U-Pb年龄谐和图;d.18-MO谐和的岩浆结晶锆石年龄图

      Fig.  5.  Zircon U-Pb concordia diagrams for the quartz syenites in the Tietang Gorge, West Qinling

      图  6  西秦岭铁堂峡脉岩标准矿物QAP图解

      Streckeisen et al.(1967)

      Fig.  6.  QAP diagram for the dykes in the Tietang Gorge, West Qinling

      图  7  西秦岭铁堂峡脉岩主量元素SiO2-K2O图(a);A/NK-A/CNK图解(b)

      a.据Rollinson(1993);b.据Maniar and Piccoli.(1989)

      Fig.  7.  SiO2 vs. K2O plot (a); A/NK vs. A/CNK plot (b) for the dykes in the Tietang Gorge, West Qinling

      图  9  西秦岭铁堂峡脉岩主量元素哈克图解

      Fig.  9.  Harker diagrams of major elements for the dykes in the Tietang Gorge, West Qinling

      图  8  西秦岭铁堂峡石英正长斑岩稀土元素配分图(a)与微量元素蛛网图(b)

      球粒陨石和原始地幔标准化数据引自Sun and McDonough(1989)

      Fig.  8.  Chondrite-normalized REE patterns (a) and primitive mantle-normalized spider diagram (b) for the quartz syenites in the Tietang Gorge, West Qinling

      图  10  铁堂峡石英正长斑岩捕获锆石与围岩板岩中碎屑锆石年龄频谱图

      围岩锆石数据王元元等(2014)

      Fig.  10.  Age spectrum of xenocrystic zircons for the quartz syenites and detrital zircons from its wall rock in Tietang Gorge

      图  11  西秦岭铁堂峡石英正长斑岩La/Sm-La图解

      Fig.  11.  La/Sm vs. La plot for the quartz syenites in the Tietang Gorge, West Qinling

      图  12  秦岭西部铁堂峡石英正长斑岩微量元素哈克图解

      Fig.  12.  Harker diagrams of trace elements for the quartz syenites in the Tietang Gorge, West Qinling

      图  13  西秦岭铁堂峡石英正长斑岩(La/Yb)N-YbN图解(a)、Sr/Y-Y图解(b)、Sr/Y-(La/Yb)N图解(c)和Sr-CaO图解(d)

      a, b.据Defant and Drummond(1990);c, d.据He et al.(2011)

      Fig.  13.  (La/Yb)N vs.YbN (a), Sr/Y vs.Y (b), Sr/Y vs. (La/Yb)N (c), Sr vs. CaO (d) diagrams for the quartz syenites in the Tietang Gorge, West Qinling

      图  14  秦岭西部印支早期中酸性岩体稀土元素配分图(a)与微量元素蛛网图(b)

      球粒陨石和原始地幔标准化数据引自Sun and McDonough(1989);铁堂峡石英正长斑岩数据来自本文,其余数据来自Guo et al.(2012)杨朋涛等(2013)刘春花等(2014)Luo et al.(2015)张永明等(2017)Wang et al.(2019)

      Fig.  14.  Chondrite-normalized REE patterns (a) and primitive mantle-normalized spider diagram (b) for the Early Indosinian magmatic rocks in the West Qinling

      图  15  秦岭西部印支早期岩体锆石Hf同位素特征

      铁堂峡石英正长斑岩数据来自本文,其余数据来自杨朋涛等(2013)Guo et al.(2012)Luo et al.(2012, 2015)

      Fig.  15.  Zircon Hf isotope for the Early Indosinian magmatic rocks in the West Qinling

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