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.
出处
《云南地质》
2014年第2期214-218,共5页
Yunnan Geology
关键词
斑岩铜钼矿
矿化特征
控矿条件
云南宾川小龙潭
Porphyry Cu-Mo Deposit
Metallogenetic Feature
Ore Control Conditions
Xiaolongtan, Binchuan, Yunnan
