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江西九岭杂岩体中黑云母花岗闪长岩年龄及对扬子和华夏板块碰撞拼合时间限定

张志辉, 张达, 贺晓龙, 胡擘捷, 祝新友, 杜泽忠, 贾文彬, 巩小栋. 2021. 江西九岭杂岩体中黑云母花岗闪长岩年龄及对扬子和华夏板块碰撞拼合时间限定[J]. 中国地质, 48(5): 1562-1579. doi: 10.12029/gc20210518
引用本文: 张志辉, 张达, 贺晓龙, 胡擘捷, 祝新友, 杜泽忠, 贾文彬, 巩小栋. 2021. 江西九岭杂岩体中黑云母花岗闪长岩年龄及对扬子和华夏板块碰撞拼合时间限定[J]. 中国地质, 48(5): 1562-1579. doi: 10.12029/gc20210518
ZHANG Zhihui, ZHANG Da, HE Xiaolong, HU Bojie, ZHU Xinyou, DU Zezhong, JIA Wenbin, GONG Xiaodong. 2021. Biotite granodiorite age of Jiuling complex in Jiangxi Province and its limitation on the collision and splicing time of the Yangtze and Cathay plates[J]. Geology in China, 48(5): 1562-1579. doi: 10.12029/gc20210518
Citation: ZHANG Zhihui, ZHANG Da, HE Xiaolong, HU Bojie, ZHU Xinyou, DU Zezhong, JIA Wenbin, GONG Xiaodong. 2021. Biotite granodiorite age of Jiuling complex in Jiangxi Province and its limitation on the collision and splicing time of the Yangtze and Cathay plates[J]. Geology in China, 48(5): 1562-1579. doi: 10.12029/gc20210518

江西九岭杂岩体中黑云母花岗闪长岩年龄及对扬子和华夏板块碰撞拼合时间限定

  • 基金项目:
    国家自然科学基金项目(41772069)及中国地质调查局项目(1212011220737、121201004000150015、DD20190570)联合资助
详细信息
    作者简介: 张志辉, 1980年生, 男, 博士生, 主要从事矿床学和矿产勘查学等方面的研究工作; E-mail: zzh1102114@126.com
    通讯作者: 张达, 1967年生, 男, 教授, 博士生导师, 主要从事区域成矿学研究; E-mail: zhangda@cugb.edu.cn
  • 中图分类号: P588.12;P597

Biotite granodiorite age of Jiuling complex in Jiangxi Province and its limitation on the collision and splicing time of the Yangtze and Cathay plates

  • Fund Project: Supported by National Natural Science Foundation of China (No.41772069) and the project of China Geological Survey (No.1212011220737, No.121201004000150015, No.DD20190570)
More Information
    Author Bio: ZHANG Zhihui, born in 1980, male, doctor candidate, engaged in mineral deposits and mineral exploration. E-mail: zzh1102114@126.com .
    Corresponding author: ZHANG Da, male, born in 1967, doctoral supervisor, professor, engaged in regional metallogeny research; E-mail: zhangda@cugb.edu.cn
  • 为探讨赣北地区九岭岩体的岩浆成因和构造属性,本文选取作为九岭岩基重要组成部分的大湖塘黑云母花岗闪长岩进行了年代学、地球化学及锆石Lu-Hf同位素研究。LA-ICP-MS锆石U-Pb定年结果表明黑云母花岗闪长岩形成于(835.6±1.5)Ma,属于钾-高钾钙碱性过铝质花岗岩系列,具有典型的S型花岗岩的特点,其形成与中元古界双桥山群的熔融密切相关。锆石εHft)主要为正值(2.8~8.2),表明形成花岗岩的岩浆来源于元古宙地壳物质的再循环。大湖塘黑云母花岗闪长岩形成的构造环境背景很可能是同碰撞向后碰撞转换的阶段,结合前人研究,我们认为扬子板块和华夏板块碰撞拼合的时间上限应为835 Ma左右。

  • 加载中
  • 图 1  赣北大湖塘钨多金属矿床在华南(a)和江西省(b, 据黄兰椿和蒋少涌,2012)的大地构造位置及其地质简图(c,据项新葵等,2012

    Figure 1. 

    图 2  大湖塘石门寺钨矿段4线地质剖面图

    Figure 2. 

    图 3  大湖塘黑云母花岗闪长岩产出特征及岩石标本照片

    Figure 3. 

    图 4  大湖塘黑云母花岗闪长岩锆石阴极发光图像

    Figure 4. 

    图 5  大湖塘黑云母花岗闪长岩锆石U-Pb年龄谐和图

    Figure 5. 

    图 6  黑云母花岗闪长岩主量元素判别图

    Figure 6. 

    图 7  黑云母花岗闪长岩的微量元素蛛网图(a)和稀土元素配分曲线(b)

    Figure 7. 

    图 8  大湖塘黑云母花岗闪长岩εHf(t)-t图解

    Figure 8. 

    图 9  大湖塘黑云母花岗岩成因类型判别图解(a,据李献华,1999)

    Figure 9. 

    图 10  大湖塘黑云母花岗闪长岩的源岩判别图解(据Sylvester,1998

    Figure 10. 

    图 11  大湖塘黑云母花岗闪长岩构造环境判别图(底图据Pearce et al., 1984

    Figure 11. 

    表 1  黑云母花岗闪长岩(DHB-01)LA-ICP-MS锆石定年分析结果

    Table 1.  LA-ICP-MS zircon dating result for the biotite granodiorite

    下载: 导出CSV

    表 2  黑云母花岗闪长岩主量元素(%)、微量元素(10-6)分析结果

    Table 2.  Major (%) and trace (10-6) elements compositions of the biotite granodiorite

    下载: 导出CSV

    表 3  大湖塘黑云母花岗闪长岩Lu-Hf同位素组成

    Table 3.  Zircon Hf isotopic composition of the Dahutang biotite granodiorite

    下载: 导出CSV
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出版历程
收稿日期:  2019-10-11
修回日期:  2019-11-29
刊出日期:  2021-10-25

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