吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (2): 482-498.doi: 10.13278/j.cnki.jjuese.201602115
刘永江1,2, 刘宾强1,2, 冯志强1, 温泉波1, 李伟民1, 张铁安3, 李小玉3, 杜兵盈3
Liu Yongjiang1,2, Liu Binqiang1,2, Feng Zhiqiang1, Wen Quanbo1, Li Weimin1, Zhang Tiean3, Li Xiaoyu3, Du Bingying3
摘要：
鄂伦春自治旗老道口闪长质岩体位于兴蒙造山带东段、大兴安岭中北段,原定义为老道口单元的老道口岩体主要由闪长岩、石英二长岩和闪长玢岩组成。锆石SIMS U-Pb定年测定闪长岩年龄为(126.09±0.95)Ma,属于早白垩世岩浆活动的产物,并非前人认为的形成于寒武纪。闪长岩的w(SiO2)为56.13%~57.91%,w(TiO2)为0.97%~0.99%,w(MgO)和w(TFe2O3)分别为2.00%~2.12%和6.73%~7.41%,Mg#值为36.00~38.00,w(Na2O)为4.29%~4.53%,w(K2O)为1.38%~1.59%,K2O/Na2O为0.31~0.37,w(Al2O3)为17.95%~18.36%,相对富钠高铝,稀土元素球粒陨石标准化曲线显示其具有富含轻稀土元素(LREE)、贫重稀土元素(HREE)以及Eu(0.85~0.87)弱负异常的特点。老道口闪长岩强不相容元素Th、U、K显著富集和高场强元素Nb、Ta明显亏损,其岩浆源区可能为俯冲流体交代的岩石圈地幔。闪长岩富集Ba、K、Rb、Th、U等大离子亲石元素,高场强元素Nb、Ta、Ti、P等明显亏损,指示了与俯冲作用相关的地球化学特征。结合老道口岩体地球化学特点和区域构造背景,认为该岩体很可能形成于蒙古-鄂霍茨克洋闭合造山后的岩石圈伸展构造环境。
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