摘要
本文对四川江油龙潭子下－中三叠统界线剖面的稀土元素含量作了测试和分析。结果表明，界线层内有不同程度的稀土元素富集，其含量较上覆、下伏地层为高，且显示出Ｃｅ、Ｅｕ的负异常。
Contents of REE in the Lower-Middle Triassic boundary section in Longtanzi,Jiangyou, Sichuan were measured and analysed. REE got enrichments in the boundary bed, which has relatively high contents than those in its overlying and underlying beds,showing the negative anomalies of Ce and Eu.
出处
《西南工学院学报》
1999年第1期37-39,共3页
Journal of Southwest China Institute of Technology
关键词
三叠统
界线
稀土元素
地球化学
Lower Middle Triassic boundary
rare earth element(REE)
geological event
Longtanzi
