宾川小龙潭斑岩铜钼矿矿化特征及控矿条件  

THE METALLOGENETIC FEATURE AND ORE CONTROL CONDITIONS OF XIAOLONGTAN PORPHYRY CU-MO DEPOSIT,BINCHUAN

作　　者：张金学 罗洪昌 刘利超 杨枝斌 田锐锋 

机构地区：[1]云南省有色地质局三一〇队,云南大理671000

出　　处：《云南地质》2014年第2期214-218,共5页Yunnan Geology

摘　　要：区域性的程海深大断裂是该区的导岩、导矿构造,直接控制了富碱性斑岩和次级构造的展布,富碱性斑岩又是区内铜钼矿化的直接成矿因素,所以应重视沿北东向构造—岩浆带的找矿工作。The rock derivation, ore derivation structure in this area is Chenghai regional megafault, which directly control the distribution of porphyry rich in alkali and subordinate structure. And the porphyry rich in alkali is the direct metallogenetic factor of Cu-Mo metallogenesis in this area. Therefore, we must pay attention to the prospecting along the NE structure magmatic zone.

关 键 词：斑岩铜钼矿 矿化特征 控矿条件 云南宾川小龙潭 

分 类 号：P618.41[天文地球—矿床学]