南秦岭太平沟铜(金)矿相关花岗岩体锆石U-Pb年代学及岩石成因

张凯, 王居里, 汪佩佩, 刘文建, 王飞, 张望, 胡洋, 陈亚伟, 周兴龙, 臧斐. 2020. 南秦岭太平沟铜(金)矿相关花岗岩体锆石U-Pb年代学及岩石成因. 西北地质, 53(4): 73-85. doi: 10.19751/j.cnki.61-1149/p.2020.04.007
引用本文: 张凯, 王居里, 汪佩佩, 刘文建, 王飞, 张望, 胡洋, 陈亚伟, 周兴龙, 臧斐. 2020. 南秦岭太平沟铜(金)矿相关花岗岩体锆石U-Pb年代学及岩石成因. 西北地质, 53(4): 73-85. doi: 10.19751/j.cnki.61-1149/p.2020.04.007
ZHANG Kai, WANG Juli, WANG Peipei, LIU Wenjian, WANG Fei, ZHANG Wang, HU Yang, CHEN Yawei, ZHOU Xinglong, ZANG Fei. 2020. Zircon U-Pb Geochronology and Petrogenesis of Taipinggou Copper (Gold)-related Granites, South Qinling. Northwestern Geology, 53(4): 73-85. doi: 10.19751/j.cnki.61-1149/p.2020.04.007
Citation: ZHANG Kai, WANG Juli, WANG Peipei, LIU Wenjian, WANG Fei, ZHANG Wang, HU Yang, CHEN Yawei, ZHOU Xinglong, ZANG Fei. 2020. Zircon U-Pb Geochronology and Petrogenesis of Taipinggou Copper (Gold)-related Granites, South Qinling. Northwestern Geology, 53(4): 73-85. doi: 10.19751/j.cnki.61-1149/p.2020.04.007

南秦岭太平沟铜(金)矿相关花岗岩体锆石U-Pb年代学及岩石成因

  • 基金项目:

    陕西地矿集团有限公司地质科研专项“东秦岭(陕西)印支期—燕山期构造体制转换过程中岩浆活动与成矿作用综合研究”项目(KY201806),陕西省地勘基金“陕西省镇安县银洞弯—张子坪铅锌多金属矿预查”项目(61201405268)

详细信息
    作者简介: 张凯(1982-),男,北京市人,高级工程师,从事区域地质矿产调查与矿产勘查工作。E-mail:zhangkai1663@163.com
  • 中图分类号: P618.51

Zircon U-Pb Geochronology and Petrogenesis of Taipinggou Copper (Gold)-related Granites, South Qinling

  • 太平沟铜(金)矿床位处秦岭造山带南秦岭印支期褶皱带与老牛山-胭脂坝燕山期北东向构造岩浆岩带交汇的构造结合部位,与矿化相关的蚀变岩体呈似椭圆状,地表出露面积为0.12 km2;蚀变岩体以石英闪长岩、细粒花岗岩为主,局部可见有斑状花岗岩,其中石英闪长岩、细粒花岗岩与铜(金)矿化具有密切的成生关系。锆石的LA-ICP-MS U-Pb年代学研究表明,太平沟矿化石英闪长岩成岩年龄为(223.2±2.9)Ma,表明其侵位于晚三叠世,指示本地区铜(金)矿化成矿时代为印支晚期。岩石地球化学分析表明,石英闪长岩具有富钾(Na2O/K2O=1.21~1.75)和富碱(Na2O+K2O=7.31%~9.67%)的特点,属高钾钙碱性系列准铝质岩石;岩石的稀土元素总量较高,具明显负Eu异常,稀土配分模式呈明显右倾型;微量元素以Ba、U、K等大离子亲石元素富集,Nb、P、Ti等高场强元素亏损为特点,属于I型花岗岩。综合分析认为,太平沟铜(金)矿床为印支晚期岩浆活动的产物,暗示南秦岭宁陕—镇安地区存在重要的印支晚期岩浆成矿事件。
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收稿日期:  2019-10-21
修回日期:  2020-06-21

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