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Fig. 7

image

Ratio plots for different meteorites and minerals: irradiated spectrum divided by the virgin spectrum. Irradiations are performed with He+ (panel A)) and Ar+ (panel B)) ions. Tagish Lake spectra are from Vernazza et al. (2013). Olivine data, black and gray respectively, from Fu et al. (2012) and Loeffler et al. (2009). OC Epinal meteorite and terrestrial olivine laser ablated spectra come from Brunetto et al. (2006, 2007).

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