well, neither am I, really. But when saying Geological, I think of rocks... so the "solid matter" part. It's probably not apropriate to make such a division, though...
Well, there will be small differences in composition between different types of rock, but your four main groups of materials are:
Iron (and the elements that combine easily with it chemically), which has a density on the order of 8 g/cc. (I'm actually used to talking about these things in kg/m^3, but the program uses g/cc, so I'll go with that. "Six of one, half a dozen of the other", as my Dad says.)
Rocks (Silicon, and the elements that combine with it. I've heard that in systems with low concentrations of oxygen to start with, carbon might become the dominant building block for the "rocks" rather than silicon, but I think I've also heard that there wouldn't be much difference in density), which have a density of around 3 g/cc.
Ices (Water, Ammonia, Methane, etc, depending on temperature), which have a density around 1 g/cc.
Gas (Which, for the purposes of planetary structure, means a 75:25 H-He mix, as no other gas is likely to form a large part of the mass of a planet), which, by definition, doesn't have a well-defined density.
Ok. You already got Ice covering and water covering, I'm afraid the only thing more I can throw in currently is rock/gas ratio. I'll put that in for you.
Great! That will give me a fair bit of insight into what's going on.
Ice or water "coverings" tell me about the surface conditions of a planet, but for all I know the 100% ice covering on a planet only goes 5 or 10 km deep, and constitutes less than 1% of the mass. Furthermore, I'm seeing "Ice planets" with earthlike densities, and "rock planets" with ice-world densities. (Also, "Ice" vs "water" covering is more a difference of surface conditions than structure. The chemical is the same, and the density is almost identical. The only difference is temperature. When I talk about the difference between an "Ice" and a "rock" planet, I'm talking about the difference between "Icy crust and mantle with a rocky core (if any)" and "Rocky crust and mantle with an iron core (if any)". Titan, for instance, is an ice world, and its inhabitants (if any) would see Earth as a planet inhabited by lava monsters.).
I'm a bit confused by the Rock/Gas ratio. Are you sure it's not Rock/Gas/Ice? There's definitely a density change happening in solid planets around the ice line, and I'd assume it would be a change in the Rock/Ice ratio. Whatever is causing it, I would like to see that in the interface as well.
I see that I have to study the accrete code a bit more thouroughly. I have no Idea how it behaves on the time axis.
Oh. BTW. One thing I'm noticing in the red dwarf systems, is that they do tend to have lots of "martian" planets that should have fairly dense atmospheres at their mass, but don't (Eg, several earth masses, temperatures in the mid double-digits kelvin, but only the faintest traces of an atmosphere). My gut instinct is that, if red dwarves are less inclined to forming planets, the rock/ice portion of those planets would be smaller, but the gas portion would certainly be larger. At the very least, even if they aren't collecting hydrogen, anything that massive will certainly have a Earth/Titan-like or better atmosphere of nitrogen, et al, just from geological outgassing, which is where the atmospheres of Earth, Venus, Mars, and Titan come from. Only gas-giant atmospheres (H, He) are collected from off-planet. All other atmospheres are what's been belched out and hasn't yet escaped or reacted chemically with solids/liquids on the surface. Furthermore, my educated guess is that for a given temperature and mass, a planet massive/cold enough to retain H and He would be likely to retain more in the vicinity of a red dwarf than near a hotter star (because red dwarves wouldn't have stellar winds and radiation clearing their disks so aggressively). In short: Alot of the "Martian" worlds we see in the program would IRL be a bit more "Titanian" (Cold, thick atmosphere).
Also: I've noticed quite a few solid planets that strike me as being a bit too close to the orbits of massive Jovians in the same system. (OTOH, this can happen if there's a stable resonance like the 3:2 one between Neptune and Pluto, and such a setup could be very interesting).
Another issue that's more of an aesthetic than realistic one (In fact, it might be downright unrealistic, though we don't have any empirical data on moons outside our own Solar System), is that I'd like to see some Jovians with downright massive (Eg, Earth-mass or so) moons. Most should still be fairly-low mass, but the sci-fi geek in me loves the thought of a habitable planet orbiting a Sudarsky II giant.