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    内蒙古赤峰金厂沟梁地区花岗岩类年代学、地球化学与Hf同位素特征

    杨帆 庞雪娇 吴猛 刘淼 陈井胜 李斌

    杨帆, 庞雪娇, 吴猛, 刘淼, 陈井胜, 李斌, 2019. 内蒙古赤峰金厂沟梁地区花岗岩类年代学、地球化学与Hf同位素特征. 地球科学, 44(10): 3209-3222. doi: 10.3799/dqkx.2019.204
    引用本文: 杨帆, 庞雪娇, 吴猛, 刘淼, 陈井胜, 李斌, 2019. 内蒙古赤峰金厂沟梁地区花岗岩类年代学、地球化学与Hf同位素特征. 地球科学, 44(10): 3209-3222. doi: 10.3799/dqkx.2019.204
    Yang Fan, Pang Xuejiao, Wu Meng, Liu Miao, Chen Jingsheng, Li Bin, 2019. Geochronology, Geochemistry and Hf Isotopic Compositions of Granitoids in Jinchanggouliang Area, Chifeng, Inner Mongolia. Earth Science, 44(10): 3209-3222. doi: 10.3799/dqkx.2019.204
    Citation: Yang Fan, Pang Xuejiao, Wu Meng, Liu Miao, Chen Jingsheng, Li Bin, 2019. Geochronology, Geochemistry and Hf Isotopic Compositions of Granitoids in Jinchanggouliang Area, Chifeng, Inner Mongolia. Earth Science, 44(10): 3209-3222. doi: 10.3799/dqkx.2019.204

    内蒙古赤峰金厂沟梁地区花岗岩类年代学、地球化学与Hf同位素特征

    doi: 10.3799/dqkx.2019.204
    基金项目: 

    国家重点研发专项 2017YFC0601306

    中国地质调查局项目 DD20190042-04

    详细信息
      作者简介:

      杨帆(1987—), 男, 博士研究生, 主要从事矿产地质研究

      通讯作者:

      吴猛(1974—), 高级工程师

    • 中图分类号: P581

    Geochronology, Geochemistry and Hf Isotopic Compositions of Granitoids in Jinchanggouliang Area, Chifeng, Inner Mongolia

    • 摘要: 内蒙古赤峰金厂沟梁地区出露的中生代花岗岩类对确定华北克拉通北缘中段中生代构造格局和演化具有重要意义.对西台子岩体、金厂沟梁岩体、小西沟岩体及西对面沟岩体进行了锆石U-Pb(LA-ICP-MS)年龄测定、地球化学分析及Hf同位素测定.西台子岩体及金厂沟梁岩体锆石U-Pb测年结果分别为220.5±2.1 Ma和225.5±1.7 Ma,为晚三叠世,两个岩体具有右倾的球粒陨石标准化配分曲线,均为弱的正Eu异常,锆石εHft)的变化范围分别为-8.0~-3.0和-5.7~-2.3;小西沟岩体的锆石U-Pb测年结果为162.5±1.6 Ma,为晚侏罗世,(La/Yb)N比值为0.14~0.51,其稀土元素球粒陨石标准化图谱显示稍向左倾的"V"字型,弱的负Eu异常,锆石εHft)为-7.3~-4.4;西对面沟岩体锆石U-Pb测年结果为128.2±1.1 Ma,为晚白垩世,具有右倾的球粒陨石标准化配分曲线,弱的正Eu异常,锆石εHft)为-11.4~-10.4.西台子及金厂沟梁岩体为I型花岗岩,小西沟岩体为A1型花岗岩,西对面沟岩体为C型埃达克质岩石,其源区均为华北克拉通下地壳物质的部分熔融;西台子岩体、金厂沟梁岩体可能形成于古亚洲洋闭合后地壳伸展的动力学背景之下,小西沟岩体形成于蒙古-鄂霍茨克海闭合后的伸展构造背景,西对面沟岩体形成于地壳减薄过程中局部加厚的构造背景之下.

       

    • 图  1  金厂沟梁地区地质简图

      段培新等(2014)修改

      Fig.  1.  Sketch geological map of the Jinchanggouliang area

      图  2  金厂沟梁花岗岩类显微岩相学特征(正交偏光)

      a.西台子二长花岗岩;b.金厂沟梁二长花岗岩;c.小西沟正长花岗岩;d.西对面沟石英二长岩. Qtz.石英;Kfs.钾长石;Pl.斜长石;Bt.黑云母;Hbl.角闪石;Spn.榍石

      Fig.  2.  Characteristic photomicographs of granitoids from Jinchanggouliang(orthogonal polarization)

      图  3  典型锆石CL图像

      a.西台子岩体;b.金厂沟梁岩体;c.小西沟岩体;d.西对面沟岩体

      Fig.  3.  CL images of typical zircons

      图  4  锆石U-Pb年龄谐和曲线图

      a.西台子岩体;b.金厂沟梁岩体;c.小西沟岩体;d.西对面沟岩体

      Fig.  4.  U-Pb concordia diagrams of zircons

      图  5  金厂沟梁花岗岩类SiO2-(Na2O+K2O)图解(a); SiO2-K2O图解(b); Na2O-K2O图解(c);A/CNK-A/NK图解(d)

      图a据Irvine and Baragar(1971); 图b据Pecerillo and Taylor(1976); 图d据Maniar and Piccoli(1989)

      Fig.  5.  Plots of total alkali versus SiO2 (TAS) (a), SiO2 versus K2O (b), Na2O versus K2O(c) and A/CNK versus A/NK (d)

      图  6  金厂沟梁花岗岩类球粒陨石标准化稀土元素配分图(a)和原始地幔标准化微量元素蛛网图(b)

      图a据Boynton(1984); 图b据Sun and McDonough(1989)

      Fig.  6.  Chondrite-normalized REE patterns (a) and primitive mantle-normalized trace element spider diagram (b) for granitoids in Jinchanggouliang

      图  7  金厂沟梁地区花岗岩成因类型判别图解

      A, I, S, M分别代表A型, I型, S型, M型花岗岩;A1.大陆板内/裂谷环境; A2.造山后环境;底图a, b据Whalen et al.(1987);底图c据Chappell and White(1992);底图d, e据Eby(1992)

      Fig.  7.  Genitic type discrimination diagrams for granites in Jinchanggouliang area

      图  8  金厂沟梁地区花岗岩类锆石εHf(t)-t图解

      Fig.  8.  Diagrams of zircon εHf(t)-t of granitoids in Jinchanggouliang area

      图  9  赤峰地区花岗岩类构造环境判别图解

      Pearce et al.(1984)

      Fig.  9.  Discrimination diagram for tectonic settings from Chifeng granitoids

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