| 东天山尖山铜矿床地质特征及成矿规律 |
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| 引用本文： | 古学伟,郭全. 东天山尖山铜矿床地质特征及成矿规律[J]. 新疆地质, 2007, 25(3): 274-278 |
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| 作者姓名： | 古学伟 郭全 |
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| 作者单位： | 1. 新疆维吾尔自治区兵团国土局,新疆,乌鲁木齐,830002
2. 新疆维吾尔自治区有色黄金建设公司,新疆,乌鲁木齐,830000 |
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| 摘 要： | 尖山铜矿位于塔里木板块觉罗塔格晚古生代沟弧带南缘,赋矿地层为下石炭统白鱼山组,含矿岩性为安山质凝灰岩.矿体受康古尔塔格深大断裂之分支断裂苦水大断裂形成的低序次层间断裂破碎带控制,矿体形态为细长脉状.近矿围岩蚀变主要为绿帘石化、绿泥石化、阳起石化、黄铁矿化及绢云母化等,成因类型为中-低温热液石英脉型.
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| 关 键 词： | 东天山 铜矿床 地质特征 成矿规律 找矿标志 |
| 文章编号： | 1000-8845（2007）03-274-05 |
| 修稿时间： | 2007-04-28 |
GEOLOGICAL CHARACTERISTICS AND METALLOGENY OF EAST TIANSHAN MOUNTAIN JINSHAN |
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| GU Xue-Wei,GUO Quan. GEOLOGICAL CHARACTERISTICS AND METALLOGENY OF EAST TIANSHAN MOUNTAIN JINSHAN[J]. Xinjiang Geology, 2007, 25(3): 274-278 |
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| Authors: | GU Xue-Wei GUO Quan |
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| Affiliation: | 1. Bureau of Land and Mineral Resources, Xinjiang Army of Production and Construction, Urumuqi, Xinjiang 830002,China; 2. Xinjiang Coloured Gold Build Company, Urumuqi, Xinjian,830000, China |
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| Abstract: | Jinshan copper mine is located South Juelaotage latePaleozoic trench-island arc belt of Tarim plate,The copper mine is produced in the andesitic tuff formation of the below Carboniferous Baiyushan Formation . It is controlled by the sub-class fault of Kushui big distributive fault derived by Kuguertage big fault. ore body is slightness nervation. It's near minerals wall rock alteration include epidotization,chloritization,actinolitization,pyritization,sericitization and so on. The genetic type belong epithermal middle-low temperature quartz vein copper mine. |
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| Keywords: | copper mine Geloogical characteristics metallogeny prospecting indicator East tianshan |
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