摘要
受基性、中碱性岩体控制,多金属矿均产于喜马拉雅期碱性正长岩带岩体与断裂交汇的复合部位,矿化与构造关系密切,且以Cu-Mo为中心,向Pb-Zn-金过渡。找矿靶区可分为高、中、低温三类。
The multimetallic deposit,which is controlled by the basic,intermediate-alkaline rock body,is in the composite part of conjunction of rock body in Himalayan alkaline syenite zone and fault.The metallogenesis is in close relation with the structure,transitional from the Cu-Mo center to the Pb-Zn-Au.The prospecting targets can be divided into 3 types of high,middle and low T.
出处
《云南地质》
2012年第2期166-170,152,共6页
Yunnan Geology
关键词
金铜钼多金属矿
碱性正长岩带
断裂岩体交汇部
喜马拉雅期
云南金平平安寨
Au-Cu-Mo Multimetallic Deposit
Alkaline Syenite Zone
Conjunction Part of Fault and Rock body
Himalayan
Pinganzhai,Jinping,Yunnan
