| 金平阿德博铜镍矿区王家寨矿段矿床成因探讨 |
| |
| 引用本文： | 韦文彪,肖元元,沈良.金平阿德博铜镍矿区王家寨矿段矿床成因探讨[J].云南地质,2011,30(3):285-288. |
| |
| 作者姓名： | 韦文彪 肖元元 沈良 |
| |
| 作者单位： | 云南黄金矿业集团公司勘查院,昆明,650216 |
| |
| 摘 要： | 矿床与华力西期超基性一基性一中性岩浆杂岩关系密切，成矿专属性明显。先期矿浆在杂岩体中初步熔离富集，后期矿浆在压力作用下沿断裂贯入，经期后热液改造再富集成矿。
|
| 关 键 词： | 铜镍矿 相变带外侧 片理化断裂带 深部贯入成矿 云南金平阿德博 |
A PROBE INTO THE GENESIS OF WANGJIAZHAI ORE BLOCK OF ADEBO CU- NI OREFIELD, JINPING |
| |
| WEI Wen-biao,XIAO Yuan-yuan,SHEN Liang.A PROBE INTO THE GENESIS OF WANGJIAZHAI ORE BLOCK OF ADEBO CU- NI OREFIELD, JINPING[J].Yunnan Geology,2011,30(3):285-288. |
| |
| Authors: | WEI Wen-biao XIAO Yuan-yuan SHEN Liang |
| |
| Institution: | WEI Wen-biao,XIAO Yuan-yuan,SHEN Liang(Exploration Institute of Yunnan Au Mining Group,Kunming 650216) |
| |
| Abstract: | The ore deposit is in a close relation to the Variscan ultrabasic - basic - intermediate magmatic complex, with clear metallogenetic specialization. The earlier ore magma is immiscibly separated and concentrated preliminarily in the complex. The later one injectes in the fault under the pressure, then concentration and metal- logenesis take place after the post- hydrothermal reformation, |
| |
| Keywords: | Cu - Ni Deposit Outer Side of Facies Change Zone Schistositized Fault Zone Metallogenesisof Deep Ore Magma Injection Adebo Jinping Yunnan |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
