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Nanostructures and micro infra red behavior of black opal from Gracias, Honduras

机译:洪都拉斯格拉西亚斯的黑蛋白石的纳米结构和微红外行为

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This paper reports nanostructural and microinfrared data of a black opal from Gracias, Honduras. The opal is hosted in a volcanoclastic rock, as the cement among glass shards and as the filling material of steam vesicles (100-400 mu m in diameter). It is amorphous (opal-A), inclusions-free and consist of silica spheres, 450 nm in diameter, arranged in ordered close-packed fcclattice, producing intense play of color effects. The observation of thin sections under the polarizing light microscope reveals that the Honduran opal is characterized by pleochroism and sharp birefringence, together with striae, "twins" and zoning. Electron microscopy revealed that all these features are due to sphere packing mistakes. "Twins" and striae are due to changes in the close-packed planes stacking, whereas zoning is related to a preferential concentration of point defects (i.e., vacant silica spheres) at the opal/glass boundary. Microinfrared spectrometry indicates that the Honduran opal is closely associated with minor CO_2, possibly infiltrating among silica spheres
机译:本文报道了来自洪都拉斯格拉西亚斯的黑蛋白石的纳米结构和微红外数据。蛋白石位于火山碎屑岩中,作为玻璃碎片中的水泥和蒸汽囊(直径为100-400微米)的填充材料。它是无定形的(蛋白石A),不含杂质,由直径为450 nm的二氧化硅球组成,排列成有序的密排小块,产生强烈的色彩效果。在偏光显微镜下观察薄切片,发现洪都拉斯蛋白石具有多色性和尖锐的双折射特征,并带有条纹,“扭曲”和分区。电子显微镜显示所有这些特征是由于球体堆积错误所致。 “孪生”和条纹是由于紧密堆积的平面堆叠中的变化而引起的,而分区则与蛋白石/玻璃边界处的点缺陷(即,空的二氧化硅球)的优先集中有关。显微红外光谱分析表明,洪都拉斯蛋白石与少量CO_2密切相关,可能渗透到二氧化硅球中

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