| 东帕米尔"层控碳酸岩型"铁铜金矿浅释 |
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| 引用本文： | 王永新.东帕米尔"层控碳酸岩型"铁铜金矿浅释[J].新疆地质,2004,22(4):370-373. |
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| 作者姓名： | 王永新 |
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| 作者单位： | 新疆维吾尔自治区有色地质勘查局物探队,新疆,乌鲁木齐,830011 |
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| 摘 要： | 东帕米尔“层控碳酸岩型”铁铜金矿,形成于中元古代裂谷构造环境,产于中深变质相与中浅变质相转换部位,塔昔达坂群底部.矿床属海底喷流(含火山喷流)沉积成因,为菱铁矿和细碎屑岩-碳酸盐岩夹少量火山岩的沉积建造.铁铜金矿显示出上铁锰下铜金的元素垂向分带,构成新疆一个有希望的成矿区域.
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| 关 键 词： | 东帕米尔 层控碳酸岩型 铁铜金矿 |
| 文章编号： | 1000-8845(2004)04-370-04 |
| 修稿时间： | 2004年4月12日 |
THE PRELIMINARY STUDY OF THE STRATABOUND CARBONATE IRON-COPPER-GOLD DEPOSIT BELT IN EASTERN PAMIR |
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| WANG Yong-xin.THE PRELIMINARY STUDY OF THE STRATABOUND CARBONATE IRON-COPPER-GOLD DEPOSIT BELT IN EASTERN PAMIR[J].Xinjiang Geology,2004,22(4):370-373. |
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| Authors: | WANG Yong-xin |
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| Abstract: | The stratabound carbonate iron-copper-gold belt in the Eastern Pamir was formed in the Lower Taxidban group in a Mid Proterozoic rift. The deposits formed on the sea floor as sedimentary exhalative deposits (including volcanic exhalative sedimentation).The sediments are composed of siderite,clastic carbonates and volcanic rocks.The iron-copper- gold ores have vertical zonation with iron and manganese in the upper zone and copper and gold in the lower zone. It is a very important mineral region of Xinjiang. |
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| Keywords: | iron-copper-gold deposit stratabound carbonate Eastern Pamir |
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