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Fig. 3


Summary of ATPM chi-square fitting results to the thermal-infrared observations of (1620) Geographos obtained in 1983 using a fixed maximum equatorial diameter of 5.04 ± 0.07 km. The possible thermal inertia distribution (left) and the co-variance with thermal inertia of the average roughness fraction (right) derived at the 3σ confidence level for the three different shape models (legend).

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