冯晓燕, 张蓓莉. 青海软玉的成分及结构特征[J]. 宝石和宝石学杂志, 2004, 6(4): 7-9.
引用本文: 冯晓燕, 张蓓莉. 青海软玉的成分及结构特征[J]. 宝石和宝石学杂志, 2004, 6(4): 7-9.
FENG Xiao-yan, ZHANG Bei-li. Study on Compositions and Texture Characteristics of Nephrite from Qinghai Province[J]. Journal of Gems & Gemmology, 2004, 6(4): 7-9.
Citation: FENG Xiao-yan, ZHANG Bei-li. Study on Compositions and Texture Characteristics of Nephrite from Qinghai Province[J]. Journal of Gems & Gemmology, 2004, 6(4): 7-9.

青海软玉的成分及结构特征

Study on Compositions and Texture Characteristics of Nephrite from Qinghai Province

  • 摘要: 青海软玉矿床产于中酸性侵入岩与大理岩接触带中。其主要矿物为透闪石。利用X射线粉晶衍射、电子探针等测试手段,对软玉的矿物成分、化学成分进行了研究分析。通过对青海软玉显微结构的观察与研究,按其主要矿物透闪石组分的表现形式,较为系统地划分青海软玉的主要结构类型为:毛毡状结构、显微纤维隐晶质结构、显微纤维结构、显微叶片状隐晶质结构、显微叶片状结构以及放射状纤维结构。

     

    Abstract: Nephrite deposits in Qinghai Province have occurred in contact belt between intermediate-acidic intrusive rocks and dolomite-marble. The main mineral of Qinghai nephrite is tremolite. Using the X-ray powder diffraction, the electronic probe, etc, the mineral compositions and chemical compositions of the nephrite are analyzed. The texture can be systematically classified as the six types: the felt-like texture, the micro-fibrous cryptocrystalline texture, the micro-fibrous texture, the micro-leaf-like cryptocrystalline texture, the micro-leaf-like texture and the radiated fibrous texture.

     

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