云南镇沅黄草岭铅锌矿控矿因素及成因分析  

AN ANALYSIS OF GENESIS AND ORE CONTROL FACTOR OF HUANGCAOLING PB-ZN DEPOSIT IN ZHENYUAN,YUNNAN

作　　者：王承平[1] 施忠良[1] 刘晓燕[1] 田云[1] 廖镜明 

机构地区：[1]云南省地质矿产勘查院玉溪地质矿产所,云南玉溪653100

出　　处：《云南地质》2012年第4期456-459,共4页Yunnan Geology

摘　　要：矿区位于兰坪-普洱中生代前陆盆地南端,景星组下段上部浅色细碎屑岩夹钙锰质层为赋矿岩层,矿床严格受断层及破碎带控制,属典型的沉积改造中低温铅锌矿床。The orefield is in the S end part of Lanping - Puer Mesozoic foreland basin. The ore - bearing bed is the pale - color fine clastic rock with intercalation of Ca - Mn layer of upper part of Jingxing Formation Lower Member. The ore deposit is controlled strictly by the fault and fracture zone. It is a typical mid -low T Pb -Zn de- posit of sedimentation reformation.

关 键 词：中低温铅锌矿 沉积改造型 景星组下段上部 地表矿化带找矿 云南镇沅黄草岭 

分 类 号：P618.41[天文地球—矿床学] P618.42[天文地球—地质学]