吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (2): 374-388.doi: 10.13278/j.cnki.jjuese.201502104
汪岩1, 付俊彧1, 杨帆1, 那福超1, 陈会军1, 张昱2, 杨晓平3, 张铁安2
Wang Yan1, Fu Junyu1, Yang Fan1, Na Fuchao1, Chen Huijun1, Zhang Yu2, Yang Xiaoping3, Zhang Tiean2
摘要:
黑龙江省嫩江至黑河一带发育大量的晚古生代花岗岩类岩石,同位素测年结果显示主要集中在3个时代:早石炭世、晚石炭世和早二叠世。岩石类型从花岗闪长岩-二长花岗岩-正长花岗岩-碱长花岗岩等均有不同出露,石炭纪部分岩石遭受韧性剪切变质变形作用改造形成花岗质糜棱岩。岩石整体具有高硅、富钾钠特征;稀土元素总量偏高,铕负异常明显;微量元素具明显的大离子亲石元素(LILE)K、Rb、Th富集和高场强元素(HFSE)Nb、P、Ti亏损特征。其中石炭纪花岗岩类地球化学特征显示陆缘弧及同碰撞花岗岩特点,二叠纪花岗岩则表现后造山花岗岩特点。二者反映了由碰撞造山向板内后造山阶段转变的构造环境特点,也反映了嫩江-黑河构造带汇聚拼合与伸展的活动史。
中图分类号:
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