澳大利亚紫色砾背蛋白石的矿物学及谱学特征

Mineralogical and Spectral Characteristics of Purple Boulder Opal from Australia

  • 摘要: 紫色砾背蛋白石是市场上较为新颖的宝石品种,学界目前对它的研究仅限于矿物组成及体色成因,并未对其化学成分、谱学特征、变彩成因进行较为深入的分析。对澳大利亚紫色砾背蛋白石的矿物学及谱学特征进行综合研究,结果表明,紫色砾背蛋白石的主要矿物组成为非晶态蛋白石,并含有少量的α-方石英; EMPA分析结果显示,蛋白石基质的主要成分为SiO2,达96%以上,紫外-可见光谱表征为407,480 nm附近存在吸收强度较强的吸收峰,522 nm之后全吸收; LA-ICP-MS和紫外-可见吸收光谱的测试结果显示,紫色砾背蛋白石凝结于铁质岩石的环境中,其蛋白石基质的紫色调与Fe含量存在一定的正相关性; SEM测试结果显示,紫色砾背蛋白石变彩区域的SiO2球粒直径范围为182~240 nm,球粒周围八面体空隙的大小约在63~150 nm范围,只允许波长为400~450 nm的紫色光通过,形成单彩的紫色蛋白石。

     

    Abstract: Purple boulder opal is a relatively new gem variety in the market. At present, the research that related to purple boulder opal is limited to the mineral components and the genesis of its colour. There is no in-depth analysis on the chemical compositions, spectral characteristics and causes of play-of-colour effect. The mineralogical and spectral characteristics of purple boulder opal from Australia are comprehensively studied in this paper. The results showed that the main mineral component of purple boulder opal is amorphous opal, and it contains a small amount of α-cristobalite. The results of EMPA analysis showed that the main component of opal matrix is SiO2, which is more than 96%. The UV-Vis spectrum showed that there are absorption peaks of strong absorption intensity at 407 nm and 480 nm, and totally absorbed above 522 nm. Based on the results of LA-ICP-MS and UV-Vis absorption spectra, the saturation of the purple colour of purple boulder opal is positively correlated with Fe content. SEM results showed that the diameter of SiO2 spheres in the play-of-colour effect area of the purple boulder opal is about 182-240 nm, and the octahedral space around the sphere is about 63-150 nm. Only violet light with wavelength of 400-450 nm can pass through the sphere to form the pure purple opal.

     

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