摘要
云南东南部的震旦系沉积较全,自上而下可分为(暂定地层名称):白打旗组、六差塘组、咪咪底组、新现河组、大深沟组,其中含有三层冰成岩,分别相当于中国南部地区的灯影组(留茶坡组)和陡山沱组、南沱组、大塘坡组、富禄组(莲沱组)、长安组。
The Sinian system in Southeastern Yunnan was complete in sequence. It can be divided from top to bottom into (tentative stratum names)the Baidaqi, Liuchatang, Mimidi, Xinxianhe and Dashengou Formations, in which three layers of glacigenous rocks were intercalated, responding to the Dengying For-mation(Liuchapo Formation)and Doushantuo Formations, Nantuo, Datangpo, Fulu(Liantuo) and Changan Formations in south China region respectively.
出处
《云南地质》
1992年第4期330-335,共6页
Yunnan Geology
