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我国首次发现方锑金矿
引用本文:苑保钦,田澍章.我国首次发现方锑金矿[J].矿物学报,1989,9(4):312-314.
作者姓名:苑保钦  田澍章
作者单位:黄金地质研究所 北京 (苑保钦,田澍章),黄金地质研究所 北京(陈静渝)
摘    要:方锑金矿在我国湖南平江杨山庄金矿床中首次发现。共生矿物有:自然金、辉锑矿、自然锑、毒砂、黄铁矿、车轮矿等。颗粒极细小,直径为0.02—0.05mm,灰黑色,暗淡光泽,不透明,无解理,显微硬度211—246kg/mm~2(20g)。反射色为白色,均质,反射率:63.29(405nm),63.04(480nm),63.00(546nm),62.57(589nm),61.86(656nm)。三个不同颗粒方锑金矿电子探针分析结果:Au 43.04,43.01,42.96;Sb 56.96,56.99,57.04。化学式;Au_(0.93)Sb_2。X射线粉晶分析主要谱线:3.34(60),2.99(70),2.722(60),2.362(70),2.010(100)。

关 键 词:方锑金矿  湖南

THE FIRST DISCOVERY OF AUROSTIBITE IN CHINA
Yuan Baoqin,Tian Shuzhang,Chen Jingyu Institute of Gold and Geology,Beijing.THE FIRST DISCOVERY OF AUROSTIBITE IN CHINA[J].Acta Mineralogica Sinica,1989,9(4):312-314.
Authors:Yuan Baoqin  Tian Shuzhang  Chen Jingyu Institute of Gold and Geology  Beijing
Abstract:Aurostibite 1s reported for the first time in China from the Yangshanzhu-ang gold deposit, Pingjiang, Hunan Province. Associated minerals are nativegold, stibnite, antimony, arsenopyrite, pyrite, bournonite, etc. It occurs asvery fine grains measuring 0.02-0.05mm in diamter. Aurostibite is greyish-black in colour, with dull lustre, opaque, no clea-vage, Hv=211-246kgmm~2(20g). In reflected light it is white and isotropic.Reflectivity: 63. 29 (405nm), 63. 04 (480nm), 63. 00 (546nm), 62. 57 (589nm), 61. 86(656nm).
Keywords:aurostibite  Hunan  
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