re: re: No-Water Nick
We actually have a surprising bank of data on this for Mars, although it is hidden as other sorts of information, like the relationship between magnetic anomalies and impacts, which yields a Curie-point depth, or the flexural rigidity of the crust, which yields a softening isotherm.
Are you running with Gilmore's take on this from LPSC in 2000 or have you developed this idea further or differently?
