俄罗斯奥斯泊矿区(11#矿)碧玉的宝石矿物学研究
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A study of gemological characteristics of green nephrite in Ospa 11# mining area of Russia
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    摘要:

    本文以采自俄罗斯奥斯泊矿区11#矿的碧玉样品作为研究对象,采用常规的宝石学测试、傅里叶变换红外光谱仪、扫描电子显微镜、X射线粉晶衍射仪,对其表面微观形貌、矿物组成、化学成分特征进行了较全面的研究。研究表明,俄罗斯奥斯泊11#矿区碧玉主要的矿物组成为透闪石,内含的黑色点状矿物为铬铁矿。结晶度较好,矿物结晶颗粒局部具有定向性,结构主要为毛毡状纤维交织变晶机构,使其具很高的韧性。俄罗斯奥斯泊11#矿碧玉的主要化学成分为MgO、SiO2、CaO,与透闪石类玉一致,与含铁量较高的新西兰碧玉不同,其主要矿物成分为透闪石。

    Abstract:

    Russia is the main source of green nephrite in the world, and the green nephrite in the mining area around the Baikal Lake is of great fame. Recently, a new mineral area of green nephrite around the area of the Ospa Lake was found, whose market prospect is brisk. However, the lack of study in this field makes the research work a bit hard. In this paper, characteristics of mineral compositions and chemical components of green nephrite samples form Russia were studied by means of the conventional gemmological testing, X-ray powder diffraction, electron microprobe analysis and infrared spectra. The results indicate that the microtexture of Russia green nephrite is very compact. Its main composition component is tremolite. In addition, the black impurity in it is chromite. Its texture is mainly of the felt-like fiber interwoven metacryst mechanism,so the tenacity is very high. Russian green nephrite is different from green nephrite from New Zealand in composition and microtexture.

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赵洋洋,吴瑞华,吴青蔓,等, 2014. 俄罗斯奥斯泊矿区(11#矿)碧玉的宝石矿物学研究[J]. 岩石矿物学杂志, 33(S1):37~42.
ZHAO Yang-yang, WU Rui-hua, WU Qing-man, et al, 2014. A study of gemological characteristics of green nephrite in Ospa 11# mining area of Russia[J]. Acta Petrologica et Mineralogica, 33(S1): 37~42.

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  • 收稿日期:2013-07-18
  • 最后修改日期:2013-12-18
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  • 在线发布日期: 2014-03-05
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