吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (2): 389-403.doi: 10.13278/j.cnki.jjuese.201502105
司秋亮1,2, 崔天日2, 唐振2,3, 李伟2, 吴新伟2,3, 江斌2,3, 李林川2,3
Si Qiuliang1,2, Cui Tianri2, Tang Zhen2,3, Li Wei2, Wu Xinwei2,3, Jiang Bin2,3, Li Linchuan2,3
摘要：
对大兴安岭中段柴河地区玛尼吐组火山岩进行了锆石LA-ICP-MS U-Pb年代学和岩石地球化学研究,以了解其形成时代、岩石成因及其所揭示的区域构造背景。玛尼吐组火山岩岩相学鉴定结果为安山岩、英安岩,化学成分显示其为粗面英安岩、粗面岩和英安岩。玛尼吐组火山岩锆石多呈自形半自形晶,振荡环带发育,Th/U=0.33~2.08,指示其岩浆成因。定年结果显示,玛尼吐组火山岩形成于139~148 Ma的晚侏罗世。岩石地球化学研究表明,玛尼吐组火山岩的w(SiO2)为64.87%~68.65%,w(Al2O3)为15.53%~16.72%,全碱w(Na2O+K2O)为6.75%~9.22%,K2O/Na2O=0.63~1.57,属于高钾钙碱性系列。所有样品的稀土配分曲线具有相似的特征,稀土丰度总量w(∑REE)为(124.95~208.57)×10-6,轻重稀土分馏明显,(La/Yb)N=11.50~14.88, Eu负异常(0.45~1.17),微量元素以富集Rb、Ba、K,亏损Nb、P、Ti为特征。玛尼吐组火山岩原始岩浆来源于地壳岩石的部分熔融,形成于蒙古-鄂霍茨克缝合带闭合后的岩石圈伸展构造环境。
中图分类号:
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