| 锗的重要迁移形式——锗氢化物 |
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| 引用本文： | 郑大中,郑若锋.锗的重要迁移形式——锗氢化物[J].化工矿产地质,2006,28(3):140-148. |
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| 作者姓名： | 郑大中 郑若锋 |
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| 作者单位： | 成都综合岩矿测试中心,四川,成都,610081 |
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| 摘 要： | 经对锗及其氢化物的物理化学性质、有关矿床矿物流体包裹体化学成分、主要含锗矿物及锗矿物的化学成分、内生锗矿物的共生伴生矿物特征等相关问题的研讨,认为锗氢化物、锗合金氢化物是锗成矿的重要迁移形式。
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| 关 键 词： | 锗氢化物 锗合金氢化物 迁移形式 锗矿床 |
| 文章编号： | 1006-5296(2006)03-0140-09 |
| 收稿时间： | 2005-10-12 |
| 修稿时间： | 2006-07-08 |
GERMANIUM-HYDRID: THE IMPORTANT CONVECTIVE FORMATION OF GERMNIUM |
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| Zheng Dazhong,Zheng Ruofeng.GERMANIUM-HYDRID: THE IMPORTANT CONVECTIVE FORMATION OF GERMNIUM[J].Geology of Chemical Minerals,2006,28(3):140-148. |
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| Authors: | Zheng Dazhong Zheng Ruofeng |
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| Institution: | Rocks and Ores Test Center of Chengdu, Chengdu, Sichuan, 610081, China |
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| Abstract: | Discussing the physicochemical properties on germanium and its hydride and the chemical composition of minerals fluid inclusion for the related ore deposits,as well as the studies of the chemical composition of germnium bearing minerals and germnium minerals,and perusing into characters of associate minerals of endogenesis germnium minerals. it is figured out that the important convective formation of germanium is germnium hyride and germnium alloy hydride. |
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| Keywords: | germnium hydride germanium alloy hydride convective formation germnium deposit |
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