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下扬子地区姚村A型花岗岩年代学、地球化学特征及岩石成因

王存智, 黄志忠, 赵希林, 褚平利, 黄文成, 宋世明, 徐杨, 杨超. 2021. 下扬子地区姚村A型花岗岩年代学、地球化学特征及岩石成因[J]. 中国地质, 48(2): 549-563. doi: 10.12029/gc20210214
引用本文: 王存智, 黄志忠, 赵希林, 褚平利, 黄文成, 宋世明, 徐杨, 杨超. 2021. 下扬子地区姚村A型花岗岩年代学、地球化学特征及岩石成因[J]. 中国地质, 48(2): 549-563. doi: 10.12029/gc20210214
WANG Cunzhi, HUANG Zhizhong, ZHAO Xilin, CHU Pingli, HUANG Wencheng, SONG Shiming, XU Yang, YANG Chao. 2021. Geochronology, geochemistry and petrogenesis of early Cretaceous Yaocun A-type granite in the Lower Yangtze region[J]. Geology in China, 48(2): 549-563. doi: 10.12029/gc20210214
Citation: WANG Cunzhi, HUANG Zhizhong, ZHAO Xilin, CHU Pingli, HUANG Wencheng, SONG Shiming, XU Yang, YANG Chao. 2021. Geochronology, geochemistry and petrogenesis of early Cretaceous Yaocun A-type granite in the Lower Yangtze region[J]. Geology in China, 48(2): 549-563. doi: 10.12029/gc20210214

下扬子地区姚村A型花岗岩年代学、地球化学特征及岩石成因

  • 基金项目:
    中国地质调查局项目(DD20160036,DD20190153)资助
详细信息
    作者简介: 王存智, 男, 1983年生, 高级工程师, 主要从事构造地质学研究; E-mail: 32107407@qq.com
  • 中图分类号: P588.12;P597+.3;P595

Geochronology, geochemistry and petrogenesis of early Cretaceous Yaocun A-type granite in the Lower Yangtze region

  • Fund Project: Supported by the projects of China Geological Survey(No. D20160036, No. DD20190153)
More Information
    Author Bio: WANG Cunzhi, male, born in 1983, senior engineer, engaged in the study of structural geology; Email: 32107407@qq.com .
  • 姚村岩体位于下扬子江南造山带东北端,主要由中心相的中粗粒正长花岗岩和边缘相的细粒似斑状正长花岗岩组成。本文对该岩体进行了详细的锆石U-Pb年代学、主量元素、微量元素以及Nd-Hf同位素研究。LA-ICP-MS锆石U-Pb定年表明姚村岩体的形成年龄为(127.6±1.4)Ma,为燕山晚期岩浆活动的产物。岩石地球化学研究表明姚村岩体属于A型花岗岩,具高硅、富铁,锆饱和温度高、轻重稀土分馏明显、富集Rb、Th、U、K、Pb等元素而亏损Ba、Nb、Sr和Ti等元素、铕负异常显著(Eu/Eu*=0.22~0.46)的特点。姚村岩体的全岩εNdt)值与锆石εHft)值分别变化于-6.2~-5.7和-13.9~-5.0,两阶段Nd和Hf同位素模式年龄分别为TDM2(Nd)=1439~1532 Ma和TDM2(Hf)=1508~2062 Ma,Nd同位素的模式年龄重叠于Hf同位素模式年龄。结合区域地质研究成果认为,姚村岩体可能于早白垩世古太平洋板块俯冲作用之后伸展-拉伸环境下,由中元古代地壳重熔而成。

  • 加载中
  • 图 1  大地构造位置图(a)、区域构造略图(b,据陈芳等,2014修改)及岩体地质简图(c)

    Figure 1. 

    图 2  姚村岩体野外及镜下照片

    Figure 2. 

    图 3  姚村岩体代表性锆石CL图像(a)及U-Pb年龄谐和图(b)

    Figure 3. 

    图 4  姚村岩体TAS分类图解(a)(据Middlemost, 1994)和K2O-SiO2图解(b)(据Peccerillo et al., 1976)(圆形为中粗粒正长花岗岩,正方形为细粒似斑状正长花岗岩)

    Figure 4. 

    图 5  姚村岩体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)

    Figure 5. 

    图 6  姚村A型花岗岩判别图解(底图a据Collins et al., 1982;底图b据Frost and Frost, 2011; 底图c和d据Whalen et al., 1987)(图例同图 4

    Figure 6. 

    图 7  姚村岩体岩浆过程判别图解(a)La-La/Sm图解; (b) Zr-Zr/Nb图解(图例同图 4

    Figure 7. 

    图 8  姚村岩体源岩判别图解:(a)摩尔Al2O3/(MgO+FeOT)-摩尔CaO/(MgO+FeOT)图解(据Altherr et al., 2000); (b)Al2O3/TiO2-CaO/Na2O图解(据Sylvester., 1998)(图例同图 4

    Figure 8. 

    图 9  姚村岩体全岩εNd(t)-t图解(a, 双桥山群和溪口岩群全岩Nd同位素据Chen & Jahn, 1998)和锆石εHf(t)-t图解(b,新元古代花岗岩锆石Hf同位素据Zhang & Zheng, 2013; Wang et al., 2013

    Figure 9. 

    表 1  姚村岩体中粗粒正长花岗岩(8849-1-1)LA-ICP-MS锆石U-Th-Pb同位素分析结果

    Table 1.  Zircon LA-ICP-MS U–Pb geochronology results in the Yaocun coarse-grained syenogranite

    下载: 导出CSV

    表 2  姚村岩体全岩主量元素(%)、稀土元素和微量元素含量(10-6

    Table 2.  The content of main elements (%), rare earth elements and trace elements(10-6) of the Yaocun pluton

    下载: 导出CSV

    表 3  姚村岩体全岩Sr-Nd同位素测试结果

    Table 3.  Sr-Nd isotope compositions of representative samples from the Yaocun pluton

    下载: 导出CSV

    表 4  姚村岩体(8849-1-1)锆石Hf同位素组成

    Table 4.  Hf isotopic compositions of zircon grains from the Yaocun pluton determined by LA-MC-ICP-MS

    下载: 导出CSV
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出版历程
收稿日期:  2018-10-30
修回日期:  2019-03-15
刊出日期:  2021-04-25

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