摘要
腊西山矿赋存在古生界崇山群变质岩系中,受区域性崇山西侧压扭性大断裂控制,矿(化)体分布于次级北西向断裂破碎带的矽卡岩碎裂岩内,矿化类型为矽卡岩型。
The Laxishan ore deposit is in Palaeozoic Chongshan Group metamorphic rock series,which is controlled by the regional pressure-shear megafault west of Chongshan.And the ore body is in the skarn fracture rock in the NW secondary fault fracture zone.The metallogenesis belongs to the skarn type..
出处
《云南地质》
2011年第2期144-147,共4页
Yunnan Geology
关键词
矽卡岩型
铜铅锌多金属
断裂破碎带
崇山群川塘组
云南保山腊西山
Skarn Type
Cu-Pb-Zn Metallic
Fault Fracture Zone
Chongshan Group Chuantang Formation
Laxishan
Baoshan
Yunnan
