云南兰坪县东至岩铅锌矿特征及找矿建议  

THE FEATURE OF DONGZHIYAN PB-ZN DEPOSIT AND PROSPECTING SUGGESTION IN NANPING,YUNNAN

作　　者：杨东华 谭波 尹留青 罗泽雄 

机构地区：[1]云南地矿国际矿业股份有限公司,云南昆明650051

出　　处：《云南地质》2016年第2期147-150,共4页Yunnan Geology

摘　　要：东至岩铅锌矿矿体均赋存于上三叠统三合洞组(T3s)碳酸盐岩之层间破构造碎带中,矿体产状与岩层产状大致相同,地质构造控矿作用较为明显。属非岩浆热液碳酸盐岩脉状铅锌矿床。The ore body of Dongzhiyan Pb-Zn deposit is in the interlayer structural fracture zone of Upper Triassic Sanhedong Formation （T3 s） carbonatite. The occurrence of ore body is roughly similar to that of rock bed. The ore control of geological structure is clear. It belongs to non magmatic hydrothermal carbonatite veined Pb-Zn

关 键 词：构造控矿 热液矿床 云南兰坪东至岩 

分 类 号：P618.42[天文地球—矿床学]