何燕, 杨会轩, 祖恩东. 雪硅钙石的矿物学特征研究[J]. 地质与资源, 2016, 25(4): 317-321. DOI: 10.13686/j.cnki.dzyzy.2016.04.002
    引用本文: 何燕, 杨会轩, 祖恩东. 雪硅钙石的矿物学特征研究[J]. 地质与资源, 2016, 25(4): 317-321. DOI: 10.13686/j.cnki.dzyzy.2016.04.002
    HE Yan, YANG Hui-xuan, ZU En-dong. STUDY ON THE MINERALOGICAL CHARACTERISTICS OF TOBERMORITE[J]. Geology and Resources, 2016, 25(4): 317-321. DOI: 10.13686/j.cnki.dzyzy.2016.04.002
    Citation: HE Yan, YANG Hui-xuan, ZU En-dong. STUDY ON THE MINERALOGICAL CHARACTERISTICS OF TOBERMORITE[J]. Geology and Resources, 2016, 25(4): 317-321. DOI: 10.13686/j.cnki.dzyzy.2016.04.002

    雪硅钙石的矿物学特征研究

    STUDY ON THE MINERALOGICAL CHARACTERISTICS OF TOBERMORITE

    • 摘要: 研究发现,雪硅钙石是一种硅酸钙水化物.根据电子探针分析结果计算得到的化学式为(Ca4.424K0.021Mg0.0034.448(Si5.731Al0.7286.465O16(OH)2·4H2O,与经典化学式Ca5Si6O16(OH)2·4H2O基本一致.通过X射线粉晶衍射结果分析认为,该雪硅钙石属于1.4 nm类型雪硅钙石.雪硅钙石矿物呈放射状纤维集合体,颗粒大小为0.2 mm×0.5 mm×0.3 mm,黄褐色,正低突起,最高干涉色为Ⅰ级黄,二轴晶正光性,光轴角为53°.

       

      Abstract: Tobermorite is a kind of calcium silicate hydrate. By electron microprobe analysis, the chemical formula of tobermorite from Nammaw jadeite orebody in Myanmar is(Ca4.424K0.021Mg0.003)4.448 (Si5.731Al0.728)6.465O16(OH)2·4H2O, which is almost consistent with the classic chemical formula of Ca5Si6O16(OH)·2·4H2O. The result of X-ray diffraction analysis(XRD) shows that the studied tobermorite belongs to the 1.4 nm type. Through microscopic observation, XRD and electron microprobe method, this tobermorite occurs as radial fibrous aggregate in yellowish-brown color, with low positive relief and I-order yellow interference color. The mineral is optically biaxial positive with an optic axial angle of 53°.

       

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