摘要
成矿区划分为2个金成矿带,10个金矿田。构造控矿明显,岩浆活动与金成矿关系密切,成矿具长期性和滞后性,类型多样,矿床(点)空间分布集中,金与锑(汞)关系共存,找金潜力较大。
The metallogenetic area can be divided into 2 Au metallogenetic zones, l0 Au Orefields. The structural ore control is evident, the Au metallogenesis is in close relation to the magmatism. The metallogenesis period is long, postponable. The ore deposit type is various, the distribution is concentrated. And the Au is in para- genesis with Sb （Hg） . The prospecting potentiality is good.
出处
《云南地质》
2010年第1期13-18,共6页
Yunnan Geology
关键词
金矿化集中区
10个金矿田
成矿规律明显
找矿潜力较大
滇东南
Concentration Area of Important Au Metallogenesis
10 Au Orefields
Evident Metallogenetic Rule
Good Prospecting Potentiality
SE Yunnan
