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Infrared diffuse reflectance spectra of weathered and unweathered CR2 chondrites: Comparison with asteroids

机译:风化和未风化CR2球粒陨石的红外漫反射光谱:与小行星的比较

摘要

The presence and intensity of absorption band near 3μm in the reflectance spectra are due to the presence and abundance of hydrates and/or hydroxylions. Previously, we have shown that Renazzo (CR2 chondrite) is an excellent spectral match to 2 Pallas (B-type asteroid) in the wavelength region near 3μm. In this paper, we have measured infrared diffuse reflectance spectra of eight Antarctic CR2 chondrites and have compared reflectance spectra of CR2 chondrites with those of eight asteroids which belong to the C, G, B and F taxonomic classes. The spectral absorption near 3μm of Antarctic CR2 chondrites are deepened and rounded compared to that of Renazzo (fell 1824). This difference implies the presence of corrosion products probably due to terrestrial weathering of the Antarctic CR2 chondrites. This is the reason why no asteroids has been found that has an Antarctic CR2 meteorite counterpart. In addition to the close similarity between Pallas and Renazzo, the overall spectral profile of 511 Davida also exhibit similarity to the Renazzo spectrum.
机译:反射光谱中3μm附近吸收带的存在和强度归因于水合物和/或羟基离子的存在和丰度。以前,我们已经证明,Renazzo(CR2球粒陨石)在3μm附近的波长范围内与2 Pallas(B型小行星)具有出色的光谱匹配。在本文中,我们测量了8个南极CR2球粒陨石的红外漫反射光谱,并将CR2球粒体的反射光谱与C,G,B和F分类类的8个小行星的反射光谱进行了比较。与Renazzo相比,南极CR2球粒陨石在3μm附近的光谱吸收更深和更圆(下降1824)。这种差异意味着腐蚀产物的存在可能是由于南极CR2球粒陨石的陆地风化。这就是为什么没有发现具有南极CR2陨石对应物的小行星的原因。除了Pallas和Renazzo之间的相似度外,511 Davida的总体光谱曲线也与Renazzo光谱相似。

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