| 羟钒锌铅矿在中国的首次发现与研究 |
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| 引用本文： | 丁奎首,臧启家,崔文元.羟钒锌铅矿在中国的首次发现与研究[J].地质科学,1987,0(4):358-363. |
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| 作者姓名： | 丁奎首 臧启家 崔文元 |
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| 作者单位： | 1. 中国科学院地质研究所;2. 北京大学地质系 |
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| 摘 要： | 文中之羟钒锌铅矿系国内首次发现,用化学分析、X射线法、差热、红外光谱等手段进行了研究。 矿物呈黄褐色完美的晶簇,比重6.14,成分、结构及物理性质和国外同类矿物相同。作者重点地研究了它的热相变全过程,进而指出这是一种和多金属硫化矿床有关的次生矿物。
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| 关 键 词： | 羟钒锌铅矿 正钒酸盐 热相变 次生矿物 辽宁建平 |
| 收稿时间： | 1986-07-01 |
| 修稿时间： | 1986-07-01; |
CU-DESCLOIZITE DISCOVERED AND STUDIED FOR THE FIRST TIME IN CHINA |
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| Ding Kuishou.CU-DESCLOIZITE DISCOVERED AND STUDIED FOR THE FIRST TIME IN CHINA[J].Chinese Journal of Geology,1987,0(4):358-363. |
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| Authors: | Ding Kuishou |
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| Institution: | 1. Institute of Geology, Academia Sinica, Beijing;2. Department of Geology, Beijing University, Beijing |
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| Abstract: | This paper reported Cu-descloizite discovered for the first time in China. The methods such as CHA, XRD, DTA and IRS etc., were used to study Cu-descloizite in a deep going way.Cu-descloizite occurred as orange-brown fine crystal cluster with a density (obs) of 6.14. The chemical composition, structure and physical properties are identical with those reported by other authors.The study on its structural transformation under heating was carried out for the first time in this paper.We consider that Cu-descloizite is a secondary mineral and its occurrence is closely related genetically to polymetal sulfide ore deposit. |
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| Keywords: | descloizite orthovanadate thermal transformation secondary mineral Jianping County Liaoning Province |
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