摘要
<正>普通蛋白石是在表生环境下由硅酸盐矿物风化后产生的二氧化硅胶体溶液凝聚而成,也可由热水中二氧化硅沉淀而成。本文选取粉色、绿色、和黄色三种不同颜色的蛋白石,在研究其宝石矿物学特征的基础上,利用红外光谱、粉晶X射线衍射、扫描电镜等现代测试手段探究蛋白石的微观结构与二氧化硅结晶相的关系;并利用紫外可见吸收光谱和X射线荧光光谱推断不同颜色蛋白石的致色元素。
引文
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