俄罗斯奥斯泊(7号)矿碧玉的宝石学及致色离子研究
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A study of gemological and color influencing ions of green nephrite from Ospinsk No. 7 mining area, Russia
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    摘要:

    俄罗斯碧玉进入中国市场以来,以其艳丽的颜色和细腻的质地而深受广大爱玉者的喜爱。前人对俄罗斯碧玉的研究中,样品大部分采自市场,具体产地不清,且未对水线、猫眼进行研究。本文在前人研究的基础上,运用电子探针和微量元素测试等现代测试方法对俄罗斯奥斯泊矿碧玉进行分析,并对其致色离子进行研究。结果表明,奥斯泊矿碧玉主要矿物成分为透闪石,黑色点状杂质为铬铁矿,周围含有绿泥石;水线成分为透闪石;碧玉鲜艳的绿色调主要与Cr元素含量有关,Cr元素含量在400~1 500 μg/g时,可使碧玉呈现比较鲜艳的翠绿色。

    Abstract:

    In recent years, Russian green nephrite has entered Chinese market. Its gorgeous green color and nice quality are favored by many customers. In the previous study of Russian green nephrite, most samples were collected from the market, and hence the location wasn't specific; in addition, the study of the "water line" and "cat eyes" was very insufficient. Based on previous studies, the authors employed EMPA and LA-ICP-MS to study the mineralogy of green nephrite from Ospinsk of Russia and, on such a basis, discussed its color influencing ions. The results show that the main mineral composition of Ospinsk green nephrite is tremolite, and the black spotted impurities turn out to be chromite, surrounded by chlorite. The "water line" is composed of tremolite as well. Ospinsk green nephrite's brilliant green hue is mainly related to Cr element content, which can assume bright green color in 400~1 500 μg/g.

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袁淼,吴瑞华,张锦洪, 2014. 俄罗斯奥斯泊(7号)矿碧玉的宝石学及致色离子研究[J]. 岩石矿物学杂志, 33(S1):48~54.
YUAN Miao, WU Rui-hua, ZHANG Jin-hong, 2014. A study of gemological and color influencing ions of green nephrite from Ospinsk No. 7 mining area, Russia[J]. Acta Petrologica et Mineralogica, 33(S1): 48~54.

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  • 收稿日期:2013-08-27
  • 最后修改日期:2013-12-10
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  • 在线发布日期: 2014-03-05
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