| 新疆温泉县托克赛西铅锌矿地质特征及成因浅析 |
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| 引用本文： | 邵勤国. 新疆温泉县托克赛西铅锌矿地质特征及成因浅析[J]. 甘肃冶金, 2016, 0(5): 34-37. DOI: 10.3969/j.issn.1672-4461.2016.05.012 |
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| 作者姓名： | 邵勤国 |
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| 作者单位： | 新疆有色地质勘查局地质矿产勘查研究院,新疆 乌鲁木齐,830000 |
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| 摘 要： | 矿区位于天山地槽褶皱带西段与准噶尔-阿拉套山地槽褶皱带交汇部位,处于赛里木地块捷克利-赛里木铜成矿带,是寻找层控型铅-锌多金属矿和与中酸性侵入岩有关的有色及稀有金属矿产的有利地区。铅锌矿厚度大,品位高,沉积作用明显。
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| 关 键 词： | 托克赛西 铅锌矿 矿床成因 |
Geological Features and Oregenesis of Tuokesaixi Lead-zinc Deposit in Wenquan County |
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| Abstract: | The ore field is located in the intersection of western section of the Tianshan Mountgeosyncline folding belt and the Zhungeer?Alatao Mount geosyncline folding belt, in the Jiekeli?Sailimu copper mineralization belt of Sailimu massif, is a favorite area for prospecting for strata?bound lead?zinc polymetallic deposit and nonferrous and rare?metallic deposit relavant to medium?acidic invasive rock. The lead?zinc deposit is characterized with thick orebody, high grade and obvious sedimen?tation. |
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| Keywords: | Tuokesaixi lead-zinc deposit oregenesis |
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