| 兰坪县金顶铅锌矿床地质特征及成因分析 |
| |
| 引用本文： | 宁选凤,;苏昌学.兰坪县金顶铅锌矿床地质特征及成因分析[J].云南地质,2014(4):526-531. |
| |
| 作者姓名： | 宁选凤 ;苏昌学 |
| |
| 作者单位： | [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 |
| |
| 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）相热水沉积超大型矿床。
|
| 关 键 词： | 多期成矿 陆(湖)相热水沉积矿床 云南兰坪金顶 |
THE GEOLOGICAL FEATURE AND GENESIS ANALYSIS OF JINDING PB-ZN DEPOSIT IN LANPING |
| |
| Institution: | NING Xuan-feng, SU Chang-xue ( 1. Yunnan Hongdi Company (Ltd) of Mineral Resources, Kunming 650051 ; 2. Exploration and Design Institute, Yunnan Bureau of Nonferrous Geology, Kunming 650051 ) |
| |
| Abstract: | 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. |
| |
| Keywords: | Multiperiodic Metallogenesis Land （Lake） Facies Hydrothermal Sedimentary Deposit Jind- ing Lanping Yunnan |
| 本文献已被 维普 等数据库收录！ |
|
