Oh. DGP = Digest Group Publications. Publishers of Megatraveller stuff, now decanonised because of legal dispute between Marc Miller and Roger Sanger (who now owns the rights to that material). Joe Fugate is now on these boards, he used to run the company, go see the MT board for details.
As for monazite:
http://mineral.galleries.com/minerals/phosphat/monazite/monazite.htm
Hey, it's radioactive too!
It forms in "phospatic pegmatites". IIRC that means it forms when deep underground magma chambers full of molten rock that have a lot of water (and in this case phosphates) in them cool down very slowly - the slow cooling causes the crystals that form to grow quite large, but the water in the magma causes the crystals to grow even bigger than usual as the magma solidifies.
Eventually, this gets uplifted and eroded, and then you get your monazite sand - assuming that the magma chamber that formed it had the right composition in the first place.
So if you don't get uplift and erosion, you don't get your monazite being exposed on the surface and eroded, which makes it about a zillion times harder to find it since it's buried in a magma chamber a few km below the crust that's very hard to find.
Net result - you'll probably find Lanthanum on large, tectonically active worlds, and not on small, dead rockballs.
(if you want to do it realistically, that is. You could, alternatively say that there are mountains of pur lanthanum on some wacky world or other

)