摘要
云南香格里拉县休瓦促钨钼矿,矿体均赋存于燕山期二长花岗岩体之构造裂隙或破碎带石英脉中,为石英脉型钨辉钼矿。该钨钼矿体的形成,主要与区内燕山期花岗岩浆侵入活动有关,而矿体就位又受到构造断裂裂隙的控制。
The orebody of Xiuwacu W-Mo deposit in Shanggelila,Yunnan is the structure fissure or fracture zone of quartz vein in Yanshanian adamellite,which is the quartz vein W-Mo deposit in the relation to Yanshanian granite intrusion in this area.The emplacement of orebody is controlled by the structure fault.
作者
吴艳
WU Yan(Henan Geological Museum,Zhengzhou 450016)
出处
《云南地质》
2019年第4期450-453,共4页
Yunnan Geology
