| 麻栗坡三保银多金属矿床 |
| |
| 引用本文： | 龚洪波,陈书富.麻栗坡三保银多金属矿床[J].云南地质,2005,24(3):333-339. |
| |
| 作者姓名： | 龚洪波 陈书富 |
| |
| 作者单位： | 云南省有色地质306队,昆明,650216 |
| |
| 摘 要： | 田蓬组地层成矿元素高背景值,为有利之矿源层。加里东期~印支期区域变质作用与成矿密切相关。变质热液长期、持续作用,矿源层内成矿元素随热液迁移,有利赋矿部位富集改造形成层控矿床。
|
| 关 键 词： | 银多金属矿 变质热液 层控 富集改造 三保麻栗坡云南 |
| 文章编号： | 1004-1885（2005）03-333-07 |
| 收稿时间： | 2005-05-12 |
| 修稿时间： | 2005-05-12 |
THE SANBAO AG POLYMETALLIC DEPOSIT OF MALIPO |
| |
| GONG Hong-bo,CHEN Shu-fu.THE SANBAO AG POLYMETALLIC DEPOSIT OF MALIPO[J].Yunnan Geology,2005,24(3):333-339. |
| |
| Authors: | GONG Hong-bo CHEN Shu-fu |
| |
| Institution: | Yunnan Nonferrous Geological Team 306, Kunming 650216 |
| |
| Abstract: | The Middle Cambrian Tianpeng Formation has high background value of metallogenetic element, which is the advantageous ore source horizon.The metallogenesis is close related with the Caledonian-Indosinian regional metamorphism.The protracted continuous action of metamorphic thermal fluid, the migration of metallogenetic element in ore source horizon accompanying thermal fluid, which is concentrated, reformed and became the stratabound ore deposit at the advantageous ore-bearing position. |
| |
| Keywords: | Metamorphic thermal fluid Element Migration Concentra tion-Reformation Ag Polymetallic Deposit Sanbao Malipo |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
