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桐柏—大别造山带南缘七尖峰花岗岩成因:来自地球化学、锆石U-Pb年代学和Hf同位素的制约

江拓, 邱啸飞, 卢山松, 杨红梅, 邓新, 彭练红. 2020. 桐柏—大别造山带南缘七尖峰花岗岩成因:来自地球化学、锆石U-Pb年代学和Hf同位素的制约[J]. 中国地质, 47(4): 1109-1126. doi: 10.12029/gc20200414
引用本文: 江拓, 邱啸飞, 卢山松, 杨红梅, 邓新, 彭练红. 2020. 桐柏—大别造山带南缘七尖峰花岗岩成因:来自地球化学、锆石U-Pb年代学和Hf同位素的制约[J]. 中国地质, 47(4): 1109-1126. doi: 10.12029/gc20200414
JIANG Tuo, QIU Xiaofei, LU Shansong, YANG Hongmei, DENG Xin, PENG Lianhong. 2020. Petrogenesis of the Qijianfeng granite in southern Tongbai-Dabie orogenic belt:Constraints from geochemistry, zircon U-Pb age and Hf isotope[J]. Geology in China, 47(4): 1109-1126. doi: 10.12029/gc20200414
Citation: JIANG Tuo, QIU Xiaofei, LU Shansong, YANG Hongmei, DENG Xin, PENG Lianhong. 2020. Petrogenesis of the Qijianfeng granite in southern Tongbai-Dabie orogenic belt:Constraints from geochemistry, zircon U-Pb age and Hf isotope[J]. Geology in China, 47(4): 1109-1126. doi: 10.12029/gc20200414

桐柏—大别造山带南缘七尖峰花岗岩成因:来自地球化学、锆石U-Pb年代学和Hf同位素的制约

  • 基金项目:
    国家自然科学基金项目(41902232、41303026)和中国地质调查局地质调查项目(DD20190291、DD20190050)联合资助
详细信息
    作者简介: 江拓, 男, 1987年生, 助理研究员, 岩石学专业, 主要从事造山带构造演化研究工作; E-mail:jiangtuogeology@163.com
  • 中图分类号: P541

Petrogenesis of the Qijianfeng granite in southern Tongbai-Dabie orogenic belt:Constraints from geochemistry, zircon U-Pb age and Hf isotope

  • Fund Project: Supported by National Natural Science Foundation of China (No. 41902232, No.41303026) and China Geological Survey (No. DD20190291, No.DD20190050)
More Information
    Author Bio: JIANG Tuo, male, born in 1987, assistant researcher, majors in petrology, engages in research on tectonic evolution of orogenic belts; E-mail:jiangtuogeology@163.com .
  • 以桐柏—大别造山带南缘七尖峰花岗岩体为研究对象,进行了详细的同位素年代学和元素-同位素地球化学研究,对其岩石成因和桐柏—大别造山带南缘早白垩世构造背景与钼成矿作用进行了探讨。锆石LA-ICP-MS U-Pb定年结果表明,七尖峰花岗岩形成年龄为(140±1)Ma,说明其为早白垩世岩浆活动的产物。地球化学研究表明,七尖峰花岗岩具有高SiO2(72.88%~73.60%)、低MgO(0.33%~0.36%),高Sr(620×10-6~642×10-6)、Sr/Y(107~111)比值,低Y(5.65×10-6~5.95×10-6)、Yb(0.52×10-6~0.59×10-6)、无Eu负异常的地球化学特征,是典型的埃达克岩。岩体富K2O、贫Cr和Ni,具有富集的Sr-Nd同位素组成(ISr=0.7075~0.7078,εNdt)=-15.5~-15.1),锆石εHft)值在-19.9~-13.2变化,对应的两阶段Nd和Hf模式年龄分别介于2.15~2.19 Ga和2.00~2.43 Ga,暗示七尖峰花岗岩是由古老的加厚下地壳含石榴石角闪岩部分熔融形成。结合前人的研究成果,认为桐柏—大别造山带白垩纪存在两期与钼成矿密切相关的岩浆事件,早期(>130 Ma)与加厚下地壳部分熔融有关,晚期(< 130 Ma)则形成于非加厚地壳部分熔融,证明桐柏—大别造山带南缘早白垩世(约130 Ma)经历了从碰撞挤压地壳加厚到碰撞后伸展地壳减薄的构造垮塌演化过程。

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  • 图 1  桐柏—大别造山带大地构造位置(a)和区域地质简图(b)(据Wang et al., 2014b修改)

    Figure 1. 

    图 2  七尖峰岩体地质图(据陈超等, 2018修改)

    Figure 2. 

    图 3  七尖峰花岗岩野外及镜下照片

    Figure 3. 

    图 4  七尖峰花岗岩锆石阴极发光图像(a,实线和虚线圈分别代表U-Pb年龄和Hf同位素测点,“/”两侧分别为U-Pb年龄和εHf(t)值)、LA-ICP-MS锆石U-Pb年龄谐和图(b)和加权平均年龄图(c)

    Figure 4. 

    图 5  七尖峰花岗岩主量元素成分图解

    Figure 5. 

    图 6  七尖峰花岗岩球粒陨石标准化的稀土配分模式图(a)及原始地幔标准化的多元素蛛网图(b),球粒陨石和原始地幔标准化值引自Sun and McDonough(1989)

    Figure 6. 

    图 7  七尖峰花岗岩ISr-εNd(t)图解

    Figure 7. 

    图 8  七尖峰花岗岩锆石t-εNd(t)演化图

    Figure 8. 

    图 9  七尖峰花岗岩Sr/Y-Y图解(a, Defant and Kepezhinskas, 2002)和(La/Yb)N-YbN图解(b, Drummond and Defant, 1990),图例同图 5

    Figure 9. 

    图 10  七尖峰花岗岩Al2O3-K2O/Na2O图解(a, Deng et al., 2016)及SiO2-MgO图解(b, Wang et al., 2007),图例同图 5

    Figure 10. 

    表 1  七尖峰花岗岩(17QJF01)LA-ICP-MS锆石U-Pb测试结果

    Table 1.  LA-ICP-MS zircon U-Pb analytical data for the Qijianfeng granite (17QJF01)

    下载: 导出CSV

    表 2  七尖峰花岗岩主(%)、微量(10-6)元素分析结果

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

    下载: 导出CSV

    表 3  七尖峰花岗岩Sr-Nd同位素分析结果

    Table 3.  Sr-Nd isotopic composition of the Qijianfeng granite

    下载: 导出CSV

    表 4  七尖峰花岗岩锆石Lu-Hf同位素分析结果

    Table 4.  In situ Lu-Hf isotopic data of zircon from the Qijianfeng granite

    下载: 导出CSV

    表 5  桐柏—大别造山带早白垩世与钼成矿相关花岗岩特征汇总

    Table 5.  Summary of the early Cretaceous Mo-related granites in the Tongbai-Dabie orogenic belt

    下载: 导出CSV
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出版历程
收稿日期:  2019-06-17
修回日期:  2019-10-23
刊出日期:  2020-08-25

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