The Yunlu migmatites occur in the south-eastern part of the Yunkai Caledonian orogenic belt, South China. The NE-trending belt is composed mainly of pre-Devo-nian metapelitic rocks, migmatites and large volumes of granites. The metamorphism in the area, w
陈斌 黄福生.1994.粤西云炉地区混合岩的成因研究[J].地质学报,68(3). Chen Bin, Huang Fusheng.1994. ON THE ORIGIN OF MIGMATITES IN YUNLU, WEST GUANGDONG PROVINCE[J]. Acta Geologica Sinica,68(3).
