金平平安寨金多金属矿成矿规律及找矿前景  

THE METALLOGENETIC RULE AND PROSPECTING POTENTIALITY OF PINGANZHAI AU MULTIMETALLIC DEPOSIT,JINPING

作　　者：舒培华[1] 杨昌毕[2] 李玉光[2] 

机构地区：[1]云南省地质矿产勘查开发局第二地质大队,云南文山663000 [2]云南黄金矿业集团股份有限公司勘查院,云南昆明650224

出　　处：《云南地质》2012年第2期166-170,152,共6页Yunnan Geology

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.

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 

分 类 号：P618[天文地球—矿床学]