兰坪县金顶铅锌矿床地质特征及成因分析  

THE GEOLOGICAL FEATURE AND GENESIS ANALYSIS OF JINDING PB-ZN DEPOSIT IN LANPING

作　　者：宁选凤 苏昌学 

机构地区：[1]云南弘迪矿产资源有限公司,云南昆明650011 [2]云南有色地质局勘测设计院,云南昆明650051

出　　处：《云南地质》2014年第4期526-531,共6页Yunnan Geology

摘　　要：兰坪县金顶铅锌矿体主要赋存在一个封闭的构造体系当中,早期经过成岩成矿阶段的初步富集,晚期弯窿构造形成过程中矿物质再次富集,形成了一个陆(湖)The main orebody been concentrated preliminarily in arch structure formation, resulting of Jinding Pb-Zn deposit, Lanping is in a closed structural system, which has the early rock-forming metallogenetic stage, and concentrated again in the late in the formation of a land facies （lake） hydrothermal sedimentary superlargeore deposit.

关 键 词：多期成矿 陆(湖)相热水沉积矿床 云南兰坪金顶 

分 类 号：P618.42[天文地球—矿床学]