吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (2): 417-428.doi: 10.13278/j.cnki.jjuese.201502107
张海华, 郑月娟, 陈树旺, 李永飞, 张健, 卞雄飞, 苏飞, 公繁浩, 黄欣
Zhang Haihua, Zheng Yuejuan, Chen Shuwang, Li Yongfei, Zhang Jian, Bian Xiongfei, Su Fei, Gong Fanhao, Huang Xin
摘要:
笔者对内蒙古科尔沁右翼中旗代钦塔拉地区出露的花岗质岩进行了锆石U-Pb定年和岩石地球化学研究,旨在探讨该区花岗岩成因类型和区域构造演化。研究区的花岗质岩主要以黑云母花岗岩和花岗闪长岩为主,岩石明显富SiO2、Al2O3和碱质,属于过铝质高钾钙碱性系列的S型花岗岩;稀土元素标准化配分图总体呈轻稀土富集、重稀土亏损特点,LREE/HREE的值为3.12~16.17,平均为10.07;LaN/YbN为2.72~28.71,具中等程度的负Eu异常;岩石富集大离子亲石元素Rb、K、Pb,亏损高场强元素Nb、Ta、Zr、Ce、Ti,具碰撞型花岗岩的特征。依据地球化学特征可将花岗岩划为低Sr低Yb型,说明花岗岩可能是在较高的压力下形成的。锆石U-Pb年龄为(242.6±2.5)Ma,表明该区古亚洲洋的俯冲碰撞发生在三叠纪,花岗岩体的形成与碰撞拼合有关。
中图分类号:
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