| 金川Ⅰ矿区6#富铜盲矿体成因探讨 |
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| 引用本文： | 孟蓉,田毓龙.金川Ⅰ矿区6#富铜盲矿体成因探讨[J].云南地质,2006,25(3):374-380. |
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| 作者姓名： | 孟蓉 田毓龙 |
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| 作者单位： | 1. 昆明理工大学,云南,昆明,650093
2. 昆明理工大学,云南,昆明,650093;金川镍钴研究设计院,甘肃,金昌,737102 |
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| 摘 要： | 金川硫化铜镍矿床Ⅰ矿区6#富铜矿属于岩浆深熔-晚期贯入矿体，于正常的超基性岩型富矿体之后，富含贵金属元素和铜镍的富矿岩浆沿北东东向张性断裂上侵形成，呈透镜状产出。
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| 关 键 词： | 盲矿体 铜镍硫化物矿床 成因 金川 甘肃 |
| 文章编号： | 1004-1885（2006）03-376-07 |
| 收稿时间： | 2006-03-10 |
| 修稿时间： | 2006-03-10 |
A STUDY ON THE GENESIS OF BLIND OREBODY RICH IN 6# CU OF OREFIELD Ⅰ, JINCHUAN |
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| MENG Rong,TIAN Yu-long.A STUDY ON THE GENESIS OF BLIND OREBODY RICH IN 6# CU OF OREFIELD Ⅰ, JINCHUAN[J].Yunnan Geology,2006,25(3):374-380. |
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| Authors: | MENG Rong TIAN Yu-long |
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| Abstract: | The metallogenesis of orebody rich in Cu of Jinchuan sulfide Cu-Ni deposit belongs to the type of magmatic anatexis-late injection. It is formed after the rich orebody of normal ultrabasic rock type. And the magma rich in precious metal elements and Cu-Ni intrudes upwards along the NEE tensile fault, which is in lenticulated occurrence. |
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| Keywords: | Blind Orebody Cu-Ni Sulfide Deposit Genesis Jinchuan Gan-su |
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