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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Petrography of the carbonaceous, diamond-bearing stone 'Hypatia' from southwest Egypt: A contribution to the debate on its origin
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Petrography of the carbonaceous, diamond-bearing stone 'Hypatia' from southwest Egypt: A contribution to the debate on its origin

机译:从西南埃及的碳质,钻石石“丘比塔”的岩画:对其起源的辩论贡献

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The stone named "Hypatia" found in the Libyan Desert Glass area of southwest Egypt is carbon-dominated and rich in microdiamonds. Previous noble gas and nitrogen isotope studies suggest an extraterrestrial origin. We report on a reconnaissance study of the carbonaceous matrix of this stone and the phases enclosed in it. This focused on areas not affected by numerous transecting fractures mostly filled with secondary minerals. The work employed scanning electron microscopy (SEM) with energy-dispersive (EDS) and wavelength-dispersive (WDS) electron microprobe (EMPA) analysis, Proton Induced X-ray Emission (PIXE) spectrometry and micro-Raman spectroscopy. We found that carbonaceous matrices of two types occur irregularly intermingled on the 50-500 mu m scale: Matrix-1, consisting of almost pure carbonaceous matter, and Matrix-2, containing Fe, Ni, P and S at abundances analyzable by microprobe. Matrix-2 contains the following phases as inclusions: (i) (Fe, Ni) sulphide occurring in cloud-like concentrations of sub-mu m grains, in domains of the matrix that are enriched in Fe and S. These domains have (Fe + Ni)/S (atomic) = 1.51 +/- 0.24 and Ni/Fe = 0.086 +/- 0.061 (both 1SD); (ii) grains up to similar to 5 mu m in size of moissanite (SiC); (iii) Ni-phosphide compound grains up to 60 mu m across that appear cryptocrystalline or amorphous and have (Ni + Fe)/P (atomic) = 5.6. +/- 1.7 and Ni/Fe = 74 +/- 29 (both 1SD), where both these ratios are much higher than any known Ni-phosphide minerals; (iv) rare grains (observed only once) of graphite, metallic Al, Fe and Ag, and a phase consisting of Ag, P and I. In Matrix-2, Raman spectroscopy shows a prominent narrow diamond band at 1340 cm(-1). In Matrix-1 the D and G bands of disordered carbon are dominant, but a minor diamond band is ubiquitous, accounting for the uniform hardness of the material. The D and G bands have average full width at half maximum (FWHM) values of 295 +/- 19 and 115 +/- 19 cm(-1), respectively, and th
机译:在西南埃及利比亚沙漠玻璃区发现了“丘比塔”的石头是碳统治和富含微石斛。以前的惰性气体和氮同位素研究表明外星源。我们报告了这块石头碳质基质的侦察研究及其包围的阶段。这集中在不受多种横切裂缝的区域,主要填充次级矿物质。该工作采用扫描电子显微镜(SEM),具有能量分散(EDS)和波长分散(WDS)电子微探测(EMPA)分析,质子诱导的X射线发射(PIME)光谱和微拉曼光谱。我们发现,两种类型的碳质基质发生在50-500 mu m刻度上不规则地混合:基质-1,由微探针分析的丰度,含有Fe,Ni,P和S的基质-1,包括Fe,Ni,P和S的基质-2。基质-2含有以下相含量:(i)(Fe,Ni)硫化物,硫化物样浓度的亚μm颗粒的亚mμm颗粒中,其在富含Fe和S的基质结构域中(Fe + ni)/ s(原子)= 1.51 +/- 0.24和Ni / Fe = 0.086 +/- 0.061(1SD); (ii)谷物达到类似于10μm的Moossanite(SiC); (iii)氮磷化合物粒度高达60μm,可看出加密晶或无定形的,具有(Ni + Fe)/ p(原子)= 5.6。 +/- 1.7和Ni / Fe = 74 +/- 29(两个1SD),其中这些比率远高于任何已知的Ni-磷化物矿物; (iv)石墨,金属Al,Fe和Ag的稀有晶粒(仅观察一次),以及由Ag,P和I组成的相。在基质-2中,拉曼光谱显示在1340厘米处的突出窄钻杆(-1 )。在Matrix-1中,无序碳的D和G带是显性的,但次要的钻石带普遍存在,占材料的均匀硬度。 D和G频段分别具有295 +/- 19和115 +/-19cm(-1)的半最大(fwhm)值的平均全宽度,以及

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