Journal Highlight: Nanodiamonds and silicate minerals in ordinary chondrites as determined by micro-Raman spectroscopy

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  • Published: Jul 3, 2017
  • Author: spectroscopyNOW
  • Channels: Raman
thumbnail image: Journal Highlight: Nanodiamonds and silicate minerals in ordinary chondrites as determined by micro-Raman spectroscopy

Raman spectra of silicate and carbonaceous minerals in three ordinary chondrites have been measured to improve understanding of the impact process including peak metamorphic pressures present in carbon-bearing ordinary chondrites.

Image: NASA/JPL-Caltech

Nanodiamonds and silicate minerals in ordinary chondrites as determined by micro-Raman spectroscopy

Meteoritics & Planetary Science, 2017, 52, 1146-1154
Bhaskar J. Saikia, Gopalakrishnarao Parthasarathy and Rashmi R. Borah

Abstract: We present here the Raman spectroscopic study of silicate and carbonaceous minerals in three ordinary chondrites with the aim to improve our understanding the impact process including the peak metamorphic pressures present in carbon-bearing ordinary chondites. The characteristic Raman vibrational peaks of olivines, pyroxenes, and plagioclase have been determined on three ordinary chondrites from India, Dergaon (H5), Mahadevpur (H4/5), and Kamargaon (L6). The Raman spectra of these meteorite samples show the presence of nanodiamonds at 1334–1345 cm−1 and 1591–1619 cm−1. The full-width at half maximum (FWHM) of Raman peaks for Mahadevpur and Dergaon reflect the nature of shock metamorphism in these meteorites. The frequency shift in Raman spectra might be because of shock effects during the formation of the diamond/graphite grains.

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