| 巴西卡拉加斯地区大规模铁-铜-金多金属矿床的成矿作用 |
| Received:March 28, 2013 Revised:January 25, 2014 点此下载全文 |
| 引用本文：ZENG Yong,GUO WeiMin,XIANG HongLi,YAO ChunYan,DONG YongGuan.2015.Massive Fe-Cu-Au polymetallic deposits metallogenesis in Carajás mineral province of Brazil[J].Mineral Deposits,34(4):828~841 |
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| Author Name | Affiliation | | ZENG Yong | China University of Geosciences, Wuhan 430074, Hubei, China
Nanjing Center of China Geological Survey, Nanjing 210016, Jiangsu, China | | GUO WeiMin | Nanjing Center of China Geological Survey, Nanjing 210016, Jiangsu, China | | XIANG HongLi | Nanjing Center of China Geological Survey, Nanjing 210016, Jiangsu, China | | YAO ChunYan | Nanjing Center of China Geological Survey, Nanjing 210016, Jiangsu, China | | DONG YongGuan | Nanjing Center of China Geological Survey, Nanjing 210016, Jiangsu, China |
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| 基金项目:本文得到中国地质调查局地质矿产调查评价项目"南美重要矿床地质背景成矿作用和找矿潜力研究(编号: 1212011220909)"和中央地质勘查基金境外风险勘查项目"南美地台优势矿产资源成矿规律与潜力分析(编号: 201130D6200119)"联合资助 |
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| 中文摘要:巴西卡拉加斯(Carajás)地区是世界上矿床类型最为丰富、资源聚集程度最高的成矿带之一。早期该地区以巨型的浅层富集型铁-锰矿著称,近年发现了世界上最大的铁氧化物铜-金矿床(群)。并且,该区的小型脉状铜-金(钨-锡)矿床、浅成热液型金-钯-铂矿床、沉积型锰矿床和与超基性岩石关的铬-镍矿床也很有特色。综合研究表明,这一区域发生了4期成矿作用:新太古代早期铁-锰成矿作用、新太古代晚期铜-金-铀-稀土元素成矿作用、古元古代晚期铜-金(钨-锡)成矿作用和新元古代晚期金-铜成矿作用。而后新生代的表生作用,特别是红土化去硅富集作用对其进行了富集改造,形成了卡拉加斯地区大规模铁-铜-金矿集区。 |
| 中文关键词:地质学 铁-铜-金矿床 成矿作用 卡拉加斯 巴西 |
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| Massive Fe-Cu-Au polymetallic deposits metallogenesis in Carajás mineral province of Brazil |
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| Abstract:The Carajás province of Brazil is one of the world famous metallogenic regions with various types of deposits and high concentration of minerals. It is well known for huge shallow enrichment type Fe-Mn deposits. In recent years the world's largest iron oxide Cu-Au deposits and some distinctive small vein type Cu-Au (W-Sn) deposits, epithermal Au-Pd-Pt deposits, sedimentary Mn deposits and Ni-Cr deposits related to ultrabasic rocks were discovered in this province. A comprehensive study shows that four periods of metallogenesis occurred in this region, namely early Neo-Archaeozoic Fe-Mn metallogenesis, late Neo-Archaeozoic Cu-Au-U-REE metallogenesis, late Paleoproterozoic Cu-Au(W-Sn) metallogenesis, and late Neoproterozoic Au-Cu metallogenesis. The Cenozoic supergenesis, especially laterized desilication enrichment, transformed Carajás into a large Cu-Au mineral province. |
| keywords:geology Fe-Cu-Au deposits metallogenesis Carajás Brazil |
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