滇东南卡林型金矿控矿因素及成矿规律浅析  

A PRELIMINARY ANALYSIS OF THE CONTROL FACTOR AND METALLOGENESIS RULE OF CARLIN-TYPE AU DEPOSIT IN SE YUNNAN

作　　者：陈少伟[1] 张志平 

机构地区：[1]云南黄金矿业集团股份有限公司,云南昆明650215 [2]云南省地质矿产开发局第五地质大队,云南普洱665000

出　　处：《云南地质》2015年第2期193-197,共5页Yunnan Geology

摘　　要：滇东南卡林型金矿带处于我国著名的滇、黔、桂"金三角"成矿带上,金矿形成与区内复杂的大地构造发展和时空演化关系密切。金矿床常常受构造控制,其中以不整合面控矿最为明显,其次为断裂破碎带控矿;低温Au-As-Hg-Sb地球化学组合异常表现明显;泥盆系、二叠系是最主要的容矿地层;与金矿化有关的蚀变主要为硅化、黄铁矿化,此为辉锑矿化、毒砂化和粘土化。The carlin-type Au deposit zone in SE Yunnan is in the famous Dian-Qian-Gui ＂Au-Triangle＂ metallogenesis zone in China. The metallogenesis of Au deposit is in close relation with the complicated tectonic development and time-space evolution in the area. The Au deposit is controlled often by the structure, unconformity first; fault fracture zone secondly. The low T Au-As-Hg-Sb geochemical assemblage anomaly is clear. The most principal ore-bearing strata are Devonian, Permian. The major alterations related with Au metallogenesis are silicification, pyritization; the minor ones are stibnitization, arsenopyritization and clay grouting.

关 键 词：多因素控矿 卡林型金矿 云南东南部 

分 类 号：P612[天文地球—矿床学]