吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (2): 460-476.doi: 10.13278/j.cnki.jjuese.20170096
张超1,2, 吴新伟1,2, 张渝金1,2, 郭威1,2, 权京玉3
Zhang Chao1,2, Wu Xinwei1,2, Zhang Yujin1,2, Guo Wei1,2, Quan Jingyu3
摘要: 龙江盆地是松辽盆地外围西部重要的火山断陷盆地之一,盆地内自下而上依次发育龙江组、光华组和甘河组火山岩。本文对龙江盆地火山岩进行了详细的锆石U-Pb年代学研究,结果显示:龙江组流纹岩、辉石英安岩、安山岩锆石U-Pb年龄分别为(129.7±2.4)、(129.0±2.3)和(125.6±1.3)Ma;光华组3个流纹岩锆石U-Pb年龄分别为(122.5±1.4)、(119.9±1.1)和(116.7±1.5)Ma;甘河组最年轻的锆石年龄为(114.3±2.9)Ma;显示盆地内火山岩浆活动的时限为129.7~114.3 Ma,火山岩均为早白垩世岩浆活动的产物。同时在甘河组玄武质粗面安山岩中测到多组捕获锆石年龄,反映出晚二叠世(254 Ma)、晚石炭世(302 Ma)、晚泥盆世(367 Ma)、早志留世(433 Ma)、古元古代(2 395 Ma)、新太古代(2 523 Ma)岩浆事件记录,这在一定程度上为龙江盆地存在古老结晶基底提供了证据。
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