Fig. 14.

Comparison of the results of this work with the results obtained by Khan et al. (2019) for the solar-like oscillating giants in the Kepler field and the K2 C3 and C6 fields. The surface gravities were obtained from the νmax scaling relation, while the distances and extinctions were computed with PARAM (Rodrigues et al. 2017), using the seismic parameters Δν, νmax, as well as spectroscopic (Kepler) or photometric (K2 effective temperatures and metallicities as an input.
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