| 云南鹤庆炉坪金多金属矿床地质特征及成因分析 |
| |
| 引用本文： | 李章雄,刘丽华,苏益志.云南鹤庆炉坪金多金属矿床地质特征及成因分析[J].云南地质,2012(3):301-304. |
| |
| 作者姓名： | 李章雄 刘丽华 苏益志 |
| |
| 作者单位： | 云南省有色地质局310队 |
| |
| 摘 要： | 矿床成矿物质源于斑岩及斑岩期后的岩浆热液,经内生成矿阶段的原生富集作用和表生成矿阶段的富集作用,逐步在相对有利的地质和地球化学环境构造部位富集成矿,属斑岩型中低温外接触带沿层破碎带型原生及氧化Fe-Au多金属矿床。
|
| 关 键 词： | 金多金属矿 原生及氧化富集 中低温热液型 构造—岩浆控矿 云南鹤庆炉坪 |
THE GENESIS ANALYSIS AND GEOLOGICAL CHARACTERISTICS OF LUPING AU MULTIMETALLIC DEPOSIT IN HEQING,YUNNAN |
| |
| LI Zhang-xiong,LIU Li-hua,SU Yi-zhi.THE GENESIS ANALYSIS AND GEOLOGICAL CHARACTERISTICS OF LUPING AU MULTIMETALLIC DEPOSIT IN HEQING,YUNNAN[J].Yunnan Geology,2012(3):301-304. |
| |
| Authors: | LI Zhang-xiong LIU Li-hua SU Yi-zhi |
| |
| Institution: | (Geological Team 310,Yunnan Bureau of Nonferrous Geology,Dali 671005) |
| |
| Abstract: | The metallogenetic material is mainly derived from the porphyry and the postmagmatic thermal fluid,which enriches and forms progressively the ore body in the advantageous geological and geochemical environment by the original and epigenetic enrichment.It belongs to the middle-low T original oxidation Fe-Au multimetallic deposit of porphyry type(bedding fracture zone type). |
| |
| Keywords: | Au Multimetallic Deposit Original and Oxidation Enrichment Middle-Low T Hydrothermal Type Ore Control of Structure-Magma Luping Heqing Yunnan |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
