<div>Rheology = dry mantle and dry crust, diffusion creep<br></div>Monte Carlo results for UCM simulations (Figure 10a). <div><br></div><div><div><b>Files:</b></div><div>Each line of the files (scores, thickness, enrichment factor and crustal radioelement content) corresponds to a model with given crustal parameters (crustal thickness in meters and enrichment factor) and the results obtained for this model.<div><br></div><div>Gaussian scores for the three constraints on elastic thickness are given in the files "score". To compute scores between 0 and 1, these scores have to be divided by the maximum of the corresponding gaussian (given in "Gaussian_maximum.csv": in order for the Noachian, the Southern polar cap and the Northern polar cap)</div><div><br></div><div>The file "MeltFormation" gives the difference in meters between the depth of the stagnant lid and the depth of melt formation in the Southern hemisphere. Models with present-day formation in the South are those where this difference is lower than 100 km.</div></div></div
