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Fig. 5
Difference in the [Fe/H] derived from BACCHUS and the corrected [M/H] from APOGEE, Δ[Fe/H] = [Fe/H]BACCHUS − [M/H]APOGEE, as a function of the APOGEE DR12 corrected global metallicity (denoted as [M/H]APOGEE), Teff, log g, and SNR for the APOKASC sample from top to bottom, respectively.
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