摘要
本文通过新测制个旧地区把南组(T3b)剖面(共计2900米)与云南省地质局1970年测制的鸟格组(T3n)剖面的对比发现,认为鸟格组地层应归属到把南组地层内,而把南组地层岩性显示为浅海相,沉积方向由上层至下层。
In this article, through comparing the new measured Banan Formation （T3b）profile （2900 meters in total） in Gejiu, Yunnan with the Niaoge Formation （T3n） profile measured by geological survey in yunnan province in 1970, this paper found that Niaoge Formation belonged to the Banan Formation, and the lithology of Banan Formation layer showed a neritic facies, sedimentary direction from upper to lower.
出处
《价值工程》
2014年第29期291-293,共3页
Value Engineering
关键词
云南个旧
剖面
岩性
对比
Gejiu,Yunnan
profile
lithology
comparison
