吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (1): 1-13.doi: 10.13278/j.cnki.jjuese.201701101
• 地质与资源 • 下一篇
张兴洲, 刘洋, 曾振, 张宏涛, 崔维龙
Zhang Xingzhou, Liu Yang, Zeng Zhen, Zhang Hongtao, Cui Weilong
摘要: 大兴安岭地区北部广泛发育一套早白垩世中酸性火山岩组合,这套组合下部以粗面岩-粗安岩为主,上部以流纹岩为主,二者的形成时代完全一致,锆石年龄均为130 Ma,对应的地质时代为早白垩世欧特里夫期。岩石地球化学资料表明,火山岩以富硅、碱及贫镁为特征,且轻重稀土分馏明显,都具有明显的Eu负异常,反映其同源演化的特点。火山岩时代与相邻正常沉积地层中化石组合时代的对比结果表明,这套火山岩与其上下正常沉积地层的沉积时代是连续演化的。火山岩之下南屯组的化石组合时代为早白垩世凡兰吟期,对应的数值年龄为139~132 Ma,之上大磨拐河组-伊敏组的化石组合时代为早白垩世欧特里夫期晚期芭蕾姆期,对应的数值年龄为129~125 Ma。这一证据揭示,大兴安岭北部在139~125 Ma的早白垩世期间经历了连续的沉积火山沉积作用演化过程,反映了该区当时伸展盆地的演化特点。其中,约130 Ma的火山岩是该区一次重要的区域性火山岩喷发事件。
中图分类号:
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