Department of Chemistry, University of Antwerp, BE 2610 Antwerp, Belgium.
Spectrochim Acta A Mol Biomol Spectrosc. 2010 May;75(5):1398-402. doi: 10.1016/j.saa.2010.01.006. Epub 2010 Feb 4.
Composition of the prehistoric pigments' (from Carriqueo rock shelter, Rio Negro province, Argentina) has been analysed by means of molecular spectroscopy (Fourier transform infrared (FTIR) and micro-Raman) and scanning electron microscopy (SEM) coupled to an energy-dispersive X-ray spectrometer (EDS). Red and yellow pigments were recognized as red and yellow ochre. The matrix of the pigments is composed of one or more substances. According to the matrix composition yellow and red pigments were also divided into two groups-i.e. those containing kaolinite or sulphates. Green pigment was detected as green earth, made up of celadonite as a chromophore.
采用分子光谱(傅里叶变换红外(FTIR)和微拉曼)和扫描电子显微镜(SEM)结合能量色散 X 射线光谱仪(EDS)对史前颜料(来自阿根廷里奥内格罗省的 Carriqueo 避难所)的组成进行了分析。红色和黄色颜料被鉴定为红土和黄土。颜料的基质由一种或多种物质组成。根据基质的组成,黄色和红色颜料也分为两组,即含有高岭石或硫酸盐的颜料。绿色颜料被检测为绿土,由作为发色团的绿泥石组成。