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一种“银线石”的宝石矿物学研究
引用本文:普丽华,李雪明,陈美玲,王铎.一种“银线石”的宝石矿物学研究[J].地质科学译丛,2012(1):51-55.
作者姓名:普丽华  李雪明  陈美玲  王铎
作者单位:[1]广东省珠宝玉石及贵金属检测中心,广东广州510080 [2]国土资源部矿产资源监督检测中心广州,广东广州510080 [3]中国地质大学教育部纳米矿物材料及应用工程研究中心,湖北武汉430074
摘    要:"银线石"是在广州市场上销售的一种低档宝石材料,已有检测机构将其定名为顽火辉石。为了确定其定名,为珠宝鉴定工作提供有用信息,采用常规的宝石学方法,EPMA,IR,XRD及SEM等大型仪器对"银线石"样品进行了研究与分析。结果表明,"银线石"为黑色-灰黑色,具交替闪现的金属状反光条带的特征外观,折射率为1.69(点测),摩氏硬度为5~6,密度为3.45g/cm3;主要矿物组成为斜方辉石亚种的紫苏辉石;紫苏辉石矿物的微细纤维状结构及相邻纤维带存在角度的排列方式,可能是"银线石"呈现特征外观的原因。"银线石"的外观特征和较高的密度值均属其鉴定特征,可与顽火辉石区分。

关 键 词:“银线石”  紫苏辉石  宝石矿物学特征

Study on Gemmological and Mineralogical Characteristics of "Silver Line Stone"
Authors:PU Li-hua  LI Xue-ming  CHEN Mei-ling  WANG Duo
Institution:1.Guangdong Provincial Gem & Precious Metal Testing Centre,Guangzhou 510080,China; 2.The Mineral Resources Supervision Testing Center of P.R.China Land & Resources Ministry, Guangzhou 510080,China;3.Engineering Research Center of Nano-Geomaterials of Ministry of Education,China University of Geosciences,Wuhan 430074,China)
Abstract:A kind of cheap gem material——"Silver Line Stone",which is recently sold in Guangzhou market,has been identified as enstatite by some testing institutions.In order to name this kind of stone and to provide useful information for the identification work,this paper investigates the "Silver Line Stone" samples by using the conventional gemmological methods and large-scale instruments(EPMA,IR,XRD and SEM).The results show that the "Silver Line Stone" is characterized by this appearance: black,grey black and metallic luster reflecting light band.Its refractive index is 1.69,its Mohs'hardness is 5~6,and its density is 3.45 g/cm3.It is mainly composed of hypersthene——a subspecies of orthorhombic pyroxene.The appearance of the "Silver Line Stone" may be caused by the micro-fine fiber structure of hypersthene and the angular arrangement of the contiguous fibrous bands."Silver Line Stone" could be easily distinguished from enstatite by its appearance characteristics and higher density.
Keywords:"Silver Line Stone"  hypersthene  gemmological and mineralogical characteristics
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