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    北山野马井地区泥盆纪富钾酸性岩浆岩地球化学特征及其地质意义

    许伟 徐学义 卢进才 牛亚卓 陈高潮 史冀忠 党犇 宋博 张宇轩 张乔

    许伟, 徐学义, 卢进才, 牛亚卓, 陈高潮, 史冀忠, 党犇, 宋博, 张宇轩, 张乔, 2019. 北山野马井地区泥盆纪富钾酸性岩浆岩地球化学特征及其地质意义. 地球科学, 44(8): 2775-2793. doi: 10.3799/dqkx.2019.048
    引用本文: 许伟, 徐学义, 卢进才, 牛亚卓, 陈高潮, 史冀忠, 党犇, 宋博, 张宇轩, 张乔, 2019. 北山野马井地区泥盆纪富钾酸性岩浆岩地球化学特征及其地质意义. 地球科学, 44(8): 2775-2793. doi: 10.3799/dqkx.2019.048
    Xu Wei, Xu Xueyi, Lu Jincai, Niu Yazhuo, Chen Gaochao, Shi Jizhong, Dang Ben, Song Bo, Zhang Yuxuan, Zhang Qiao, 2019. Geochronology, Petrogenesis and Tectonic Implications of Devonian High-K Acid Magmatic Rocks from Yemajing Area in Beishan Orogen. Earth Science, 44(8): 2775-2793. doi: 10.3799/dqkx.2019.048
    Citation: Xu Wei, Xu Xueyi, Lu Jincai, Niu Yazhuo, Chen Gaochao, Shi Jizhong, Dang Ben, Song Bo, Zhang Yuxuan, Zhang Qiao, 2019. Geochronology, Petrogenesis and Tectonic Implications of Devonian High-K Acid Magmatic Rocks from Yemajing Area in Beishan Orogen. Earth Science, 44(8): 2775-2793. doi: 10.3799/dqkx.2019.048

    北山野马井地区泥盆纪富钾酸性岩浆岩地球化学特征及其地质意义

    doi: 10.3799/dqkx.2019.048
    基金项目: 

    中国地质调查局地质调查项目 DD20160172

    国家自然科学基金项目 41402195

    中国地质调查局地质调查项目 DD20190092

    国家自然科学基金项目 41402097

    详细信息
      作者简介:

      许伟(1985-), 男, 博士研究生, 主要从事区域构造研究

    • 中图分类号: P597

    Geochronology, Petrogenesis and Tectonic Implications of Devonian High-K Acid Magmatic Rocks from Yemajing Area in Beishan Orogen

    • 摘要: 为了理清北山南部晚古生代构造演化过程,对野马井地区的二长花岗岩与流纹岩进行了岩石学、全岩主微量元素地球化学、锆石U-Pb年代学及Hf同位素等研究.LA-ICP-MS锆石U-Pb定年结果表明二长花岗岩与流纹岩的就位年龄分别为402.7±2.4 Ma与392.9±2.5 Ma.二者均为富钾钾质岩浆岩,呈现过铝质-强过铝质,轻重稀土弱到中等分馏且相对富集轻稀土,二长花岗岩呈现无或弱的负Eu异常,流纹岩呈现较明显的负Eu异常,二者均富集Rb、Th、U、Pb等,亏损Nb、Ta、Ba、Sr、Ti等,为I型酸性岩浆岩.二长花岗岩与流纹岩的锆石εHft)值介于-2.2~+6.8,对应Hf模式年龄(tDM2)为962~1 533 Ma;指示二者主要由中元古代陆壳物质熔融所形成.依据野马井地区泥盆纪富钾酸性岩浆岩的地球化学特征,结合该区域其他地质资料,可推测其为后碰撞构造环境的产物.

       

    • 图  1  北山南部地质概况及采样位置

      a.中亚造山带构造纲要与研究区位置图(据Zhou et al., 2018); b.北山南部地质概况及泥盆纪研究成果(据许伟等, 2018);c.野马井地区地质简图及采样位置

      Fig.  1.  Geological map of the investigation area and sampling positions

      图  2  野马井地区样品的镜下特征.

      Q.石英;Pl.斜长石;Bt.黑云母;Mc.微斜长石

      Fig.  2.  Photomicrograph of the Samples in the Yemajing area

      图  3  样品锆石阴极发光图像

      图中白色圈与黄色圈分别为U-Pb年龄与Hf同位素测点,并标注了锆石测点的U-Pb年龄结果与εHf(t)值

      Fig.  3.  The zircon CL images for the samples

      图  4  样品锆石U-Pb同位素年龄谐和图

      标准化数值据Sun and Mcdonough(1989);拉萨地块钾质岩数据来自Zhao et al.(2009), 王保弟等(2011);措勤现布嘎寺组钾质岩数据来自陈建林等(2006);燕冀辽地区钾质岩数据来自许保良等(1999)

      Fig.  4.  U-Pb concordia diagrams of the samples

      图  5  北山南部野马井地区泥盆纪酸性岩浆岩主量元素特征

      a.火山岩TAS分类图解投图(据Le Maitre, 1989);b. K2O-SiO2图解(据Peccerillo and Taylor, 1976);c. Na2O+K2O-CaO-SiO2图解(据Frost et al., 2001);d. A/NK-A/CNK图解(据Maniar and Piccoli, 1989);e. FeOT/(FeOT+MgO)-SiO2图解(据Frost et al., 2001);f. (Al2O3+CaO)/(FeOT+Na2O+K2O)—100(MgO+FeOT+Ti2O)/SiO2图解(据Sylvester, 1989);FeO=FeOT+0.899 8Fe2O3,A/CNK(摩尔比)=N(Al2O3)/[N(Na2O)+N(K2O)+N(CaO)],A/NK(摩尔比)=N(Al2O3)/[N(Na2O)+N(K2O)]

      Fig.  5.  Major element diagrams for the Devonian acidic magmatic rocks in the Yemajing area

      图  6  样品球粒陨石标准化稀土元素配分图(a, c)和原始地幔标准化微量元素蛛网图(b, d)

      Fig.  6.  Chondrite normalized REE patterns (a, c) and primitive mantle normalized spider diagram (b, d) for the samples

      图  7  野马井地区酸性岩浆岩主微量元素协变图解

      I型与S型花岗岩分异趋势依据Chappell(1999);元素分配系数依据Rollinson(1993);Pl.斜长石;Kfs.钾长石;Hb.角闪石;Bt.黑云母;Tit.榍石;Allan.褐帘石;Ap.磷灰石;Zr.锆石;Mon.独居石

      Fig.  7.  The major and trace elements relationship diagrams for the Devonian acidic magmatic rocks in the Yemajing region

      图  8  北山南部泥盆纪酸性岩浆岩在有关A型花岗岩判别图解中的投图

      a, b.分别为Nb和Zr含量对10 000×Ga/Al的图解;c.为Rb/Ba对Zr+ Ce+Y的图解;d.为(K2O+Na2O)/CaO对Zr+Nb+Ce+Y的图解(据Whalen et al., 1987);M, I, S.表示M型、I型、以及S型花岗岩;FG.分异的花岗岩;OGT.未分异的M型、I型、与S型花岗岩;双峰山花岗岩样品数据来自李舢等(2009);墩墩山流纹岩样品数据来自Guo et al.(2014, 2017); 王国强(2015)

      Fig.  8.  Devonian acidic magmatic rocks from southern Beishan plotted in discrimination diagrams for A-type granitoids.

      图  9  野马井地区泥盆纪酸性岩浆岩锆石εHf(t)-年龄图解

      ①.北山南部新元古界花岗岩;②.红柳园花岗岩;③.辉铜山花岗岩;④.北山南部二叠纪花岗岩;⑤.北山南部三叠纪花岗岩;Hf同位素数据源自于: 李舢等(2011); Li et al.(2012, 2013); Zhang et al.(2012); Mao et al.(2012b); Zhu et al.(2015); He et al.(2018)

      Fig.  9.  Diagram of εHf(t) vs. age for the Devonian acidic magmatic rocks in the Yemajing region.

      图  10  主微量元素构造判别图解

      Maniar and Piccoli (1989); Pearce et al.(1984); Pearce and Norry(1979); Pearce(1982, 1996); IAG.岛弧花岗岩;CAG.陆弧花岗岩;CCG.大陆碰撞花岗岩;POG.后碰撞花岗岩;RRG.裂谷相关的花岗岩;CEUG.大陆造陆抬升相关的花岗岩;双峰山花岗岩样品数据来自李舢等(2009);墩墩山流纹岩数据来自Guo et al.(2014, 2017)和王国强(2015);墩墩山玄武岩来自王国强(2015);辉铜山二长花岗岩数据来自赵泽辉等(2007);辉铜山钾长花岗岩数据来自李舢等(2011);红柳园埃达克岩数据来自Mao et al.(2012b)

      Fig.  10.  The major and trace element discrimination diagrams for the tectonic interpretation

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