| 王喜亮,曹芳芳,张磊,张文斌.新疆阿尔金柳树沟铜矿区地质特征及成因探讨[J].矿产勘查,2012,3(3):305-309 |
| 新疆阿尔金柳树沟铜矿区地质特征及成因探讨 |
| Geological characteristics and genesis of Liushugou copper ore area in Arjin,Xinjiang |
| 投稿时间：2011-11-07 |
| DOI： |
| 中文关键词: 阿尔金 铜矿区 地质特征 矿床成因 |
| 英文关键词: Arjin copper ore area geological characteristics deposit genesis |
| 基金项目: |
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| 摘要点击次数: 1905 |
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| 中文摘要: |
| 文章通过对柳树沟铜矿区地质特征的分析,总结了铜矿(化)体地质特征,认为铜矿化虽然在赋矿岩石及含矿构造上具多样性表现,但其含铜热液的来源具唯一性,为与石英斑岩的超浅成侵入体有关的含铜次火山热液,初步总结认为矿床成因为与次火山岩侵入活动有关的中低温热液充填型矿床。 |
| 英文摘要: |
| It is analyzed that the geological characteristics of Liushugou copper ore area, and summarized the copper ore body and copper mineralization demonstrate also in this paper. The authors consider that though copper mineralization has the various feature in the ore-bearing rocks and ore-bearing structure, the source of copper-bearing hydrothermal is unique. It is named copper-bearing sub-volcanic hydrothermal that related with ultra-hypabyssal quartz porphyry intrusions. The preliminary conclusion is that the genesis of copper ore deposits is mid-lower temperature hydrothermal filling deposit concerning with sub volcanic intrusive action. |
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