| 对雅满苏铁矿矿床成因的新认识 |
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| 引用本文： | 张洪武,谢丽霞.对雅满苏铁矿矿床成因的新认识[J].长春工程学院学报(自然科学版),2001,2(4):26-29. |
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| 作者姓名： | 张洪武 谢丽霞 |
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| 作者单位： | 1. 长春工程学院,地测系,长春,130021
2. 新疆雅满苏铁矿,哈密,839126 |
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| 摘 要： | 通过收集新疆雅满苏铁矿多年开采所揭露的地质现象，对其成因否定了以往的各种观点，并从多方面作出了更符合客观事实的重新论证，提出了该矿为一海底火山喷溢熔离型矿床。
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| 关 键 词： | 新疆 火山喷溢 熔离矿床 火山熔岩 |
| 文章编号： | 1009-8984(2001)04-0026-04 |
| 修稿时间： | 2001年10月11日 |
New views on origin of Yamansu iron deposit in Xinjiang autonomous region |
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| ZHANG Hong-wu,et al..New views on origin of Yamansu iron deposit in Xinjiang autonomous region[J].Journal of Changchun Institute of Technology(Natural Science Edition),2001,2(4):26-29. |
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| Authors: | ZHANG Hong-wu |
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| Abstract: | Based on exposured geologic phenomenon of Yamansu iron deposit in Xinjiang after being explored for many years, this paper refutes the existing viewpoints on its origin, devises new argumentation from many aspects that accords further with its nature, and raises an idea that the deposit is a volcanic extrusion-overflow melted- separate deposit on seabed. |
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| Keywords: | Xinjiang volcanic extrusion-overflow the melted-separate deposit volcanic melted rock |
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