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    幕阜山复式花岗岩体锆石年代与微量元素对伟晶岩矿床成因的限定

    李安邦 黄勤 冯超 杨细华 闫刚刚 赵子娟 董湘杰 祝明明 张金阳

    李安邦, 黄勤, 冯超, 杨细华, 闫刚刚, 赵子娟, 董湘杰, 祝明明, 张金阳, 2021. 幕阜山复式花岗岩体锆石年代与微量元素对伟晶岩矿床成因的限定. 地球科学, 46(12): 4517-4532. doi: 10.3799/dqkx.2021.065
    引用本文: 李安邦, 黄勤, 冯超, 杨细华, 闫刚刚, 赵子娟, 董湘杰, 祝明明, 张金阳, 2021. 幕阜山复式花岗岩体锆石年代与微量元素对伟晶岩矿床成因的限定. 地球科学, 46(12): 4517-4532. doi: 10.3799/dqkx.2021.065
    Li Anbang, Huang Qin, Feng Chao, Yang Xihua, Yan Ganggang, Zhao Zijuan, Dong Xiangjie, Zhu Mingming, Zhang Jinyang, 2021. Genesis of Mufushan Pegmatite Deposits Constrained by U-Pb Ages and Trace Elements of Zircon from Complex Granitic Batholith. Earth Science, 46(12): 4517-4532. doi: 10.3799/dqkx.2021.065
    Citation: Li Anbang, Huang Qin, Feng Chao, Yang Xihua, Yan Ganggang, Zhao Zijuan, Dong Xiangjie, Zhu Mingming, Zhang Jinyang, 2021. Genesis of Mufushan Pegmatite Deposits Constrained by U-Pb Ages and Trace Elements of Zircon from Complex Granitic Batholith. Earth Science, 46(12): 4517-4532. doi: 10.3799/dqkx.2021.065

    幕阜山复式花岗岩体锆石年代与微量元素对伟晶岩矿床成因的限定

    doi: 10.3799/dqkx.2021.065
    基金项目: 

    湖北省自然资源厅项目 ZRZR2019KY05

    详细信息
      作者简介:

      李安邦(1984-), 男, 工程师, 主要从事地矿勘查工作.ORCID: 0000-0002-1282-9313.E-mail: 709086621@qq.com

      通讯作者:

      张金阳, E-mail: zhangjinyang@cug.edu.cn

    • 中图分类号: P611.1

    Genesis of Mufushan Pegmatite Deposits Constrained by U-Pb Ages and Trace Elements of Zircon from Complex Granitic Batholith

    • 摘要: 江南成矿带晚侏罗世-早白垩世幕阜山复式花岗岩体内部及周缘发育多个早白垩世伟晶岩稀有金属矿床,成矿伟晶岩是否源自幕阜山复式岩体演化花岗岩浆高度分异还存在争议.幕阜山麦市等地发育含电气石、石榴石及白云母二长花岗岩,LA-ICP-MS锆石U-Pb年龄介于130~135 Ma,在误差范围内与区内大规模成矿伟晶岩年龄相当.与早期斑状黑云母二长花岗岩和白云母二长花岗岩(151~143 Ma)相比,晚期含电气石、石榴石及白云母二长花岗岩锆石具有较高的Hf、Ta、Nb、Th、U含量和较低的Th/U和Eu/Eu*比值,体现较高的演化程度,与岩石矿物组合及锆石结晶温度相一致.锆石年代与微量元素说明,幕阜山地区成矿伟晶岩可能是幕阜山复式岩体中早白垩世演化花岗岩浆进一步分异的产物.

       

    • 图  1  幕阜山区域位置示意图(a)、复式花岗岩体地质简图(b)及麦市周边岩体地质简图(c)

      b据李鹏等(2017);c据湖北省地质调查院,2013.1∶5万通城县幅、月田幅、陈家坝幅区域地质调查报告,武汉

      Fig.  1.  Location of Mufushan (a), geological map of the Mufushan composite granite pluton (b) and geological map near Maishi (c)

      图  2  幕阜山斑状黑云母二长花岗岩与电气石白云母二长花岗岩接触关系(a);电气石白云母二长花岗岩中呈线状分布的电气石(b);电气石白云母二长花岗岩与伟晶岩接触关系(c)

      a.a1为斑状黑云母二长花岗岩,a2为电气石白云母二长花岗岩;c.c1为电气石白云母二长花岗岩,c2为伟晶岩;图a中电气石呈团块状,图b中电气石呈线状;Tur.电气石

      Fig.  2.  The contacts between the porphyritic biotite monzogranite and tourmaline muscovite monzogranite at Mufushan (a); tourmaline line in the tourmaline muscovite monzogranite (b); the contacts between the tourmaline muscovite monzogranite and pegmatite (c)

      图  3  幕阜山麦市(a~d)、小坪(e)及李家段(f)二长花岗岩镜下显微照片

      Q.石英;Pl.斜长石;Kfs.钾长石;Bt.黑云母;Ms.白云母;Tur.电气石;Grt.石榴石

      Fig.  3.  Microphotographs of monzogranites at Maishi (a-d), Xiaoping (e) and Lijiaduan (f) from the Mufushan batholith

      图  4  斑状黑云母二长花岗岩(20M7⁃2)锆石CL图及U⁃Pb定年结果

      Fig.  4.  Cathodoluminescence images and U⁃Pb dating results of zircon grains from the porphyritic biotite monzogranite (20M7⁃2)

      图  5  二云母二长花岗岩(20X6⁃1)锆石CL图及U⁃Pb定年结果

      Fig.  5.  Cathodoluminescence images and U⁃Pb dating results of zircon grains from the two⁃mica monzogranite (20X6⁃1)

      图  6  石榴石白云母二长花岗岩(20M2⁃1)锆石CL图及U⁃Pb定年结果

      Fig.  6.  Cathodoluminescence images and U⁃Pb dating results of zircon grains from the garnet muscovite monzogranite (20M2⁃1)

      图  7  电气石白云母二长花岗岩(20M1)锆石CL图及U⁃Pb定年结果

      Fig.  7.  Cathodoluminescence images and U⁃Pb dating results of zircon grains from the tourmaline muscovite monzogranite (20M1)

      图  8  白云母二长花岗岩(20L2⁃1)锆石CL图及U⁃Pb定年结果

      Fig.  8.  Cathodoluminescence images and U⁃Pb dating results of zircon grains from the muscovite monzogranite (20L2⁃1)

      图  9  幕阜山花岗岩锆石稀土元素球粒陨石标准化配分图

      Fig.  9.  Chondrite-normalized REE patterns for zircon from the granites at Mufushan

      图  10  锆石微量元素与T关系图解

      Fig.  10.  Diagrams between trace elements and zircon crystallization temperatures

      图  11  锆石中不相容微量元素变化

      1.二云母二长花岗岩(132 Ma); 2.二云母二长花岗岩(142 Ma); 3.二云母二长花岗岩(151 Ma); 4.黑云母二长花岗岩; 5.石榴子石白云母二长花岗岩; 6.电气石白云母二长花岗岩; 7.白云母二长花岗岩

      Fig.  11.  Diagrams of incompatible trace elements in zircon

      图  12  锆石中微量元素比值变化

      1.二云母二长花岗岩(132 Ma); 2.二云母二长花岗岩(142 Ma); 3.二云母二长花岗岩(151 Ma); 4.黑云母二长花岗岩; 5.石榴子石白云母二长花岗岩; 6.电气石白云母二长花岗岩; 7.白云母二长花岗岩

      Fig.  12.  Diagrams of variation of trace element ratios in zircon

      表  1  幕阜山花岗岩与伟晶岩年龄统计

      Table  1.   Ages for granite and pegmatite at Mufushan

      岩体/脉体/矿体 年龄(Ma) 测试矿物 测试方法 位置 资料来源
      微斜长石-钠长石伟晶岩 133.0±2.6 铌铁矿 U-Pb 仁里矿床 Li et al., 2020
      微斜长石-钠长石伟晶岩 131.2±2.4 锆石 U-Pb 仁里矿床 Li et al., 2020
      黑云母二长花岗岩 140.7±0.7 锆石 U-Pb 仁里矿床 Li et al., 2020
      黑云母二长花岗岩 140.3±0.7 锆石 U-Pb 仁里矿床 Li et al., 2020
      二云母二长花岗岩 138.3±0.3 锆石 U-Pb 仁里矿床 Li et al., 2020
      含铌钽铁矿白云母钠长石伟晶岩 127.7±0.9 白云母 40Ar/39Ar 断峰山 李鹏等, 2017
      含绿柱石白云母钠长石伟晶岩 130.5±0.9 白云母 40Ar/39Ar 复式岩体中部 李鹏等, 2017
      黑云母二长花岗岩 151.2±1.1 锆石 U-Pb 复式岩体北部 Ji et al., 2017
      黑云母二长花岗岩 151.4±1.1 锆石 U-Pb 复式岩体南部 Ji et al., 2017
      黑云母花岗闪长岩 149.0±1.0 锆石 U-Pb 复式岩体东北部 Ji et al., 2017
      二云母二长花岗岩 131.8±1.5 锆石 U-Pb 复式岩体西北部 Ji et al., 2017
      二云母二长花岗岩 143.5±1.8 锆石 U-Pb 复式岩体中部 Ji et al., 2017
      二云母二长花岗岩脉 127.0±1.4 锆石 U-Pb 复式岩体西北部 Ji et al., 2017
      花岗闪长岩 151.5±1.3 锆石 U-Pb 复式岩体东部 Wang et al., 2014
      含黑云母二长花岗岩 148.3±1.4 锆石 U-Pb 复式岩体北部 Wang et al., 2014
      二云母淡色花岗岩 145.8±0.9 锆石 U-Pb 复式岩体中部 Wang et al., 2014
      斑状黑云母二长花岗岩 142.9±0.9 锆石 U-Pb 复式岩体南部 许畅等, 2019
      含铌钽矿伟晶岩 140.2±2.3 铌钽铁矿 U-Pb 仁里矿床 Xiong et al., 2020
      黑云母二长花岗岩 154.1±2.5 锆石 U-Pb 仁里矿床 Xiong et al., 2020
      白云母二长花岗岩 141.0±2.4 锆石 U-Pb 仁里矿床 Xiong et al., 2020
      白云母二长花岗岩 140.7±2.2 独居石 Th-Pb 仁里矿床 Xiong et al., 2020
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