河北唐河透闪石玉的宝石学特征及矿床成因

Study on Gemmological Characteristics and Ore Genesis of Nephrite from Tanghe,Hebei Province

  • 摘要: 通过电子探针、X射线粉末衍射、拉曼光谱、化学全岩分析以及显微镜镜下观察,确定了唐河透闪石玉的主要矿物组成为透闪石,透闪石的质量分数一般在80%以上,部分在95%以上,以纤维交织结构为主;杂质矿物有碳酸盐、石英、透辉石、滑石、褐铁矿等,质量分数少于20%。唐河透闪石玉相对和田玉,颗粒较粗,密度和硬度稍低,光泽稍差。通过氢、氧、硅同位素分析以及岩浆岩、围岩和矿石的稀土元素配分模式表明,其岩浆岩(花岗岩)只提供了成矿热液(H2O),Mg、Ca、Si主要来源于白云石和硅质条带或结核;通过包裹体测温推测其为中温成矿。经过分析研究,认为唐河透闪石玉为中酸性岩体与白云质大理岩的接触交代产物。

     

    Abstract: In recent years,a kind of nephrite from Tanghe has been discovered by some wonderful stone amateurs in Tanghe basins of Baoding,Hebei Province,which was called“Tangheyu”by the locals.However,it has not been studied whether the structure and quality of nephrite from Tanghe are corresponding with nephrite.In a field trip of local regional geology of the mine from Tanghe,the samples were collected.In this paper,the gemmological,mineralogical and petrology characteristics of the samples from Tanghe are systematically studied.It is roughly confirmed that the origins of nephrite from Tanghe are the contact zones between intermediate-acid granodiorite or granite and dolomitic marble,which locate in the stratum of Miwushan Group Jixian Period and Gaoyuzhuang Group Changcheng Period.

     

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