Major,trace element characteristics and zircon U-Pb SHRIMP dating of the Luyashan augite-monzonites and Yunzhongshan granites in Luliang area,Shanxi Provice indicate that the Luyashan augite-monzonites and Yunzhongshan granites belong to the post-orogenic granite.
结果表明 ,芦芽山辉石石英二长岩和云中山花岗岩在Y +Nb对Rb和Y对Nb图解中均位于板内花岗岩区 ,在花岗岩的R1-R2图解上 ,芦芽山含辉石石英二长岩位于后碰撞隆升 (post collisionuplift)花岗岩区 ,云中山花岗岩位于晚造山 (lateorogenic)花岗岩区 ,它们都属于后造山花岗岩。
Geological and Geomorphological Significances about Funiushan Tectonic Granite Belt in Qinling Orogenic Belt of China′s Central Orogenic System;
中国中央造山系秦岭造山带伏牛山构造花岗岩带的地质学与地貌学意义
