Extended Data Fig. 6: Data/forward model differences.
From: Remote detection of a lunar granitic batholith at Compton–Belkovich
(a-d) The “data minus model” residual antenna temperature (units K) at four frequencies subtracted from the Chang’e 2 data. Contours map the LP-GRS Th enhancement (after Wilson et al.7), (e) The pixon-reconstructed LP-GRS Th concentrations with contours of CE-2 3 GHz data- model values. (f) CE-2 data minus model residual antenna temperature at four frequencies as a function of surface measured Th.
