Having an idea about the formation of Debfurkhin (just a vague idea should be enough, no need to model everything in detail
) will also become extremely helpful in the future, because a single cycle of supercontinental breakup won't probably be enough to produce interesting (and realistic) topography everywhere. But if you have some idea about the formation of Debfurkhin and the associated orogens, you can "spice things up" by adding some ancient mountain ranges.
Having an idea about the formation of Debfurkhin (just a vague idea should be enough, no need to model everything in detail ) will also become extremely helpful in the future, because a single cycle of supercontinental breakup are necessary in order to generate a sufficient amount of geological history for a truly interesting topography, but since it's a bit too much effort to model all that, I recommend only actually modelling the one cycle, and using intuition to determine the effects of the others on the present-day topography of the planet.