吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (3): 627-638.doi: 10.13278/j.cnki.jjuese.201603101
• 地质与资源 • 下一篇
孔华1,2, 许明珠1,2, 张强1,2, 唐宇蔷1,2, 赵佳进1,2
Kong Hua1,2, Xu Mingzhu1,2, Zhang Qiang1,2, Tang Yuqiang1,2, Zhao Jiajin1,2
摘要:
道县虎子岩碱性玄武岩筒产出较多的辉长岩包体。用于锆石定年的辉长岩样品的岩石化学特征显示:其K2O、Fe2O3、TiO2高于其他同类样品,稀土元素、微量元素总量也相对较高,样品的K*值(2KN/(TaN+LaN))为7.60>1,显示岩浆具有亲岛弧性质,反映源区地幔受到较强的交代作用;Nb*值(2 NbN/(KN+LaN))为0.11<1,反映基性岩浆侵入时受到了地壳混染;辉长岩中的锆石具有清晰的韵律环带,Th/U值=0.91~4.35,具有岩浆锆石的特征;锆石206Pb/238U加权平均年龄为(201.50±0.53)Ma,代表了辉长岩的结晶年龄;εHf (t)值为-0.88~4.45,投点落入球粒陨石附近,暗示强烈的壳幔交换作用;Hf模式年龄平均为751 Ma,反映早期地壳对岩石源区的贡献。Hf同位素组成特征反映辉长质岩浆是在印支晚期局部拉张背景下,岩石圈上地幔上隆减压熔融的产物。
中图分类号:
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