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危地马拉灰绿色翡翠
引用本文:王铎,;龙楚,;谭钊勤.危地马拉灰绿色翡翠[J].地质科学译丛,2009(2):20-23.
作者姓名:王铎  ;龙楚  ;谭钊勤
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]广州海关,广东广州510623; [3]中国地质大学材料科学与化学工程学院,湖北武汉430074
摘    要:通过对危地马拉灰绿色翡翠样品进行常规宝石学测试、岩矿鉴定、X射线荧光光谱、X射线粉末衍射及红外光谱等分析,确定了其化学成分与硬玉的基本相同,其矿物组成以硬玉为主,含有少量的钠长石、白云母、钠云母及微量的黝帘石、金云母、榍石与方沸石等;主要为柱状、粒状变晶结构与粗粒变晶结构;红外光谱在1000-1100cm^-1范围内由于Ca,Mg等杂质元素替代Al引起vas(Si-O-Si)反对称伸缩振动致1071cm^-1处峰,与缅甸翡翠的相比有明显漂移。

关 键 词:危地马拉翡翠  矿物学  宝石学

Celadon Jadeite Jade from Guatemala
Institution:WANG Duo , LONG Chu , TAN Zhao-qin(1. Guangdong Provincial Gem & Precious Metal Testing Centre, Guangzhou 510080, China; 2.Guangzhou CIQ, Guangzhou 510623, China; 3. Faculty of Material Science and Chemical Engineering, China University of Geosciences , Wuhan 430074, China)
Abstract:A celadon jadeite jade sample from Guatemala is studied by using the conventional gemmological methods, rock-mine identify, XRF, XRD and IR. The results show that the chemical compositions of the sample are similar to that of jadeite. The main mineral component is jadeite, including a few albite,muscovite,paragonite and a small amount of zoisite, phlogopite, sphene and analcime. The structure of the sample is mainly column-like crystalloblastic, granoblastic and coarse granoblastic textures. At the range of 1 000-1 100 cm^-1 , the result of Al replaced by Ca and Mg with other impurity elements leads to the infrared spectrum at 1 071 cm^-1 caused by the antisymmetric stretch vibration of vas(Si-O-Si), which has the obvious drift when compared with that of the jadeite jade from Myanmar.
Keywords:jadeite jade from Guatemala  mineralogy  gemmology
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