Fig. 14.

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Spectral decomposition of the synthetic ice spectrum composed of eight components of pure ice samples (black line) and Gaussian noise (σ = 0.01). Panel a: synthetic spectrum along with the silicate band from 2.5 − 20 μm. Panel b: synthetic spectrum without the silicate feature and residual plot. The ENIIGMA fit is shown by the dashed green line and the ice components by the other colours. Panels c–e: small spectral ranges highlighting the contribution of shallow bands.
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