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| 新疆萨尔布拉克金矿 | |
| 引用本文： | 何照波,刘涛,杨宗,余红平.新疆萨尔布拉克金矿[J].云南地质,2007,26(2):175-182. |
| 作者姓名： | 何照波 刘涛 杨宗 余红平 |
| 作者单位： | 1. 新疆维吾尔族自治区云新勘查开发公司,阿勒泰,836100 2. 云南省煤炭地质勘查院,昆明,650011 3. 云南地矿资源股份公司曲靖公司,曲靖,655000 |
| 摘 要： | 萨尔布拉克金矿为北疆地区重要金矿之一,位于两个一级构造单元结合部位,矿床受北西向断裂破碎带控制,走向延伸长,规模大,从地表向下氧化矿、混合矿、硫化矿分带明显。明显受构造、地层及岩性控制,属构造一热液蚀变岩型微粒金矿。 |
| 关 键 词： | 断裂破碎带 热液蚀变 萨尔布拉克金矿 富蕴县 新疆 |
| 文章编号： | 1004-1885(2007)02-- |
| 收稿时间： | 2006-03-27 |
| 修稿时间： | 2006-03-27 |
THE SAERBULAKE AU DEPOSIT OF XINJIANG |
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| HE Zhao-bo,LIU Tao,YANG Zong,YU Hong-ping.THE SAERBULAKE AU DEPOSIT OF XINJIANG[J].Yunnan Geology,2007,26(2):175-182. | |
| Authors: | HE Zhao-bo LIU Tao YANG Zong YU Hong-ping |
| Institution: | 1. Yunxin Exploration Development Company ( Ltd;Ltd |
| Abstract: | The Saerbulake Au deposit is one of the most important Au deposit in North Xinjiang,which is situated in the conjunction part of two structural units of class 1.It is controlled by the NW fault fracture zone.Its extension in strike direction is long,on a large scale.The zonation of oxidized ore,mixed ore,sulfide ore is evident downwards from surface,which is controlled clearly by structure,strata and lithlogical character.It belongs to the micrograined Au deposit of structural hydrothermal alteration type. |
| Keywords: | Fault Fracture Zone Hydrothermal Alteration Saerbulake Au Deposit Fuyun County Xinjiang |
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