海纹石的宝玉石矿物学特征
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Mineralogical characteristics of copper pectolite
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    摘要:

    对产于多米尼加的海纹石样品进行了矿物学测试和分析.镜下观察显示,海纹石呈致密的纤维状结构,纤维长约0.01~0.02 mm;X射线衍射表明,海纹石样品主要由针钠钙石组成,并未检测到其它杂质成分,与能谱分析结果一致;不同色调的海纹石样品在红外光谱和紫外-可见光吸收光谱上都没有表现出本质的差别.

    Abstract:

    The mineralogical characteristics of copper pectolite samples from Dominican Republic were studied and analyzed. The observation under microscope shows that copper pectolite has a dense and fibrous structure, with the fiber length being about 0.01~0.02 mm. X-ray diffraction determination shows that there exists no other mineral phase except pectolite in the copper pectolite sample, which is in agreement with the result of energy disperse spectrum analysis. However, no conspicuous difference is observed in infrared spectra and ultraviolet-visible absorption spectra among the copper pectolite samples with different color tones.

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彭立华,秦善, 2014. 海纹石的宝玉石矿物学特征[J]. 岩石矿物学杂志, 33(s2):55~60.
PENG Li-hua, QIN Shan, 2014. Mineralogical characteristics of copper pectolite[J]. Acta Petrologica et Mineralogica, 33(s2): 55~60.

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  • 收稿日期:2014-08-29
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  • 在线发布日期: 2014-12-02
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