摘要
本文从阳岭砾岩的岩性特征、沉积构造和区域地质构造等方面分析入手，论证了阳岭砾岩是加里东造山带、同造山期磨拉石相的新认识，这对研究华南大地构造格架、演化和成矿规律，均具有重要的意义。
In this paper,the authors analyse lithological features,sedimentarystructure,and regional geologic structure of “Yangling psephyte” etc,andpoint out that“Yangling psephyte”bclongs to molasse facies of Caledoni-des. The new recognition is of great vdrlue of studying architectonic frame-work, evolution and minerogenetic regularity of the South China.
出处
《江西地质》
1994年第4期264-271,共8页
Jiangxi Geology
