吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (5): 1268-1283.doi: 10.13278/j.cnki.jjuese.201605101
• 地质与资源 • 下一篇
孙跃武1, 丁海生1, 刘欢2, 张德军3, 公繁浩3, 郑月娟3
Sun Yuewu1, Ding Haisheng1, Liu Huan2, Zhang Dejun3, Gong Fanhao3, Zheng Yuejuan3
摘要:
通过对内蒙古赤峰市广兴源乡于家北沟组模式剖面植物化石和安山质晶屑岩屑凝灰岩锆石U-Pb同位素年代学的研究,结合动物化石的分析,确认于家北沟组地质时代为中二叠世。于家北沟组植物化石以Gigantonoclea hallei Asama、Fascipteris sinensis Stockm. et Math.、Pecopteris taiyuanensis Halle、Pterophyllum daihoense Kaw.等众多华夏植物群典型分子为特征,属于典型的华夏植物群。目前,在中二叠世植物群中,从未发现有华夏和安加拉两大植物群的混生现象,这一事实进一步表明,中二叠世横亘于华北板块和佳蒙地块之间的古亚洲洋尚未闭合,在植物地理分布上起着重要的阻隔作用。
中图分类号:
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