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.
出处
《云南地质》
2014年第4期526-531,共6页
Yunnan Geology
关键词
多期成矿
陆(湖)相热水沉积矿床
云南兰坪金顶
Multiperiodic Metallogenesis
Land （Lake） Facies Hydrothermal Sedimentary Deposit
Jind- ing, Lanping, Yunnan
