| 湖南锡矿山锑矿床氧化带的自然硫 |
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| 引用本文： | 蒋永年.湖南锡矿山锑矿床氧化带的自然硫[J].矿物学报,1993(3). |
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| 作者姓名： | 蒋永年 |
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| 作者单位： | 地质矿产部天津地质矿产研究所 天津 |
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| 摘 要： | 本文研究的自然硫产于锡矿山锑矿床氧化带底部。它的特点是晶体细小且晶面众多,其外貌颇似小的球状体。有关它的研究结果将为矿物学形态学以及晶体形态与成因的联系(成因形态学)提供新的资料,
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| 关 键 词： | 自然硫 锑矿床氧化带 晶体形态学 成因 湖南 |
NATIVE SULFUR IN THE OXIDIZED ZONE OF THE XIKUANGSHAN ANTIMONY ORE DEPOSIT,HUNAN |
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| Jiang Yongnian Tianjin Institute of Geology and Mineral Resources,Tianjin.NATIVE SULFUR IN THE OXIDIZED ZONE OF THE XIKUANGSHAN ANTIMONY ORE DEPOSIT,HUNAN[J].Acta Mineralogica Sinica,1993(3). |
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| Authors: | Jiang Yongnian Tianjin Institute of Geology and Mineral Resources Tianjin |
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| Institution: | Jiang Yongnian Tianjin Institute of Geology and Mineral Resources,Tianjin,300170 |
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| Abstract: | The native sulfur crystals examined in this paper occur at the bottomof the oxidized zone of the Xikuangshan Sb deposit and they are characterizedby fine size and extremely abundant crystal faces, rather resembling smallspherulites. This study will provide new clues to the crystal morphology as well as tothe relationship between crystal form and genesis (genetomorphology) |
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| Keywords: | native sulfur oxidized zone of the antimony ore deposit crystal morphology genesis Hunan |
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