摘要
闾山花岗岩位于辽两台陷的东侧，是同源岩浆演化的多期产物。其物质源于地壳，一期结构演化规律强，是辽宁地区典型的“Ｓ”型花岗岩。
Tbe granite in Yiwulushan,located on the east sied West Liaoning syneclise,is theproduct of multiphase activities of comagma from the crust, which the first stage of textureevolution had a strong regular,so it belongs to a typical S-type granite.
出处
《辽宁地质》
1994年第1期154-164,共11页
关键词
花岗岩
地质特征
成因
Yiwulushan ultra-unit REE model S-type granite
