| 伊犁阿希矿化角砾岩筒型金矿床 |
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| 引用本文： | 王志辉,王润民.伊犁阿希矿化角砾岩筒型金矿床[J].成都理工大学学报(自然科学版),1995(1). |
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| 作者姓名： | 王志辉 王润民 |
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| 作者单位： | 成都理工学院资源与经济系 |
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| 摘 要： | 伊犁阿希金矿产于陆相火山岩一次火山岩中，受火山机构控制．深部火山热液承继性自多次复活的环型断裂上升，通过降压－沸腾－爆破－角砾岩化，形成以角砾胶结型矿石为主的矿化角砾岩筒型矿床。矿床规模大，品位高，矿化集中，属火山－次火山低温热液矿化角砾岩筒型矿床。
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| 关 键 词： | 金矿，火山一次火山热液矿床，矿化角砾岩筒，伊犁 |
THE MINERALIZED BRECCIA PIPE GOLD DEPOSITS IN AXI, ILI, XINJIANG |
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| Wang Zhihui, Wang Runmin.THE MINERALIZED BRECCIA PIPE GOLD DEPOSITS IN AXI, ILI, XINJIANG[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1995(1). |
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| Authors: | Wang Zhihui Wang Runmin |
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| Institution: | Wang Zhihui; Wang Runmin |
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| Abstract: | The Axi gold deposits are located in volcanic-subvolcanic rocks and controlled by volcanic mechanism. The deep hydrothermal fluids uplift from polyreactivated circular faults, and through decreasing pressure, boiling, exploding and brecciation, form mineralized breccia pipe deposits. The deposits are mainly compoised of breccia-cemented ores. They are great size and high grade,and belong to volcanic-subvolcanic low-temperature mineralized breccia pipe deposits. The ore bodies are concentrated. |
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| Keywords: | gold deposit volcanic-subvolcanic hydrothermal deposit mineralized breccia pipe Ili |
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