| 剑川麻栗箐铜铁矿地质特征及找矿方向 |
| |
| 引用本文： | 刘杰,李泉,杨洪,杨勇.剑川麻栗箐铜铁矿地质特征及找矿方向[J].云南地质,2012(1):63-65. |
| |
| 作者姓名： | 刘杰 李泉 杨洪 杨勇 |
| |
| 作者单位： | 云南省地质矿产勘查院大理地质矿产所 |
| |
| 摘 要： | 矿化体受区域构造断裂控制,矿床类型为中低温热液脉状铜铁矿床。地、物、化、遥综合研究显示,该区具有良好的成矿地质条件,有望进一步发展成为一个铜、铁矿的勘查开发区。
|
| 关 键 词： | 铜铁矿化体 构造热液型 中低温 找矿方向 云南剑川麻栗箐 |
THE GEOLOGICAL CHARACTERISTICS AND ORE PROSPECTING DIRECTION OF MALIQING CU-FE DEPOSIT,JIANCHUAN |
| |
| LIU Jie,LI Quan,YANG Hong,YANG Yong.THE GEOLOGICAL CHARACTERISTICS AND ORE PROSPECTING DIRECTION OF MALIQING CU-FE DEPOSIT,JIANCHUAN[J].Yunnan Geology,2012(1):63-65. |
| |
| Authors: | LIU Jie LI Quan YANG Hong YANG Yong |
| |
| Institution: | (Dali Institute of Geology&Mineral Resources,Yunnan Exploration Institute of Geology&Mineral Resources,Dali 671000) |
| |
| Abstract: | The metallogenetic body is controlled by the regional fault.The ore deposit belongs to the type of middle-low T hydrothermal veined Cu-Fe deposit.According to the comprehensive study of geological,geophysical,geochemical and remote sensing data,we think the geological conditions of metallogenesis in this area is good,which will be an exploration and development area of Cu-Fe deposit. |
| |
| Keywords: | Cu-Fe Metallogenetic Body Structural Hydrothermal Type Middle-Low T Ore Prospecting Direction Maliqing Cu Deposit |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
