摘要
相山外围加里东期花岗岩内发现石英脉型辉钼矿,受区内NW向构造及花岗斑岩控制,花岗斑岩侵入使加里东期岩体内钼活化迁移,为区内钼成矿提供能量。
Quartz vein type molybdenite is found in Caledonian granite in the periphery of Xiangshan,which is controlled by NW trending structure and granite porphyry in the area.Granite porphyry intrusion activates and migrates molybdenum in Caledonian rock mass,providing energy for molybdenum mineralization in the area.
作者
陈健平
揭伟成
黄柔睿
CHEN Jian-ping;JIE Wei-cheng;HUANG Rou-rui(Nuclear geology brigade of Jiangxi Geological Bureau,Yingtan 335000,China)
出处
《世界有色金属》
2021年第21期87-88,共2页
World Nonferrous Metals
关键词
加里东期
钼矿
石英脉
花岗斑岩
Caledonian
Molybdenum ore
Quartz vein
Granite porphyry
