Feldspar or feldspar rich granite is a good call on the pink formation. Banded iron formations are sedimentary formations so it's less likely to be directly associated with granite intrusions, but the first photo might be a partially metamorphized deposit of banded iron or an iron-rich slate layer. Shale laid down in oxygen poor conditions would have un-reduced iron which (after metamorphosis and being brought to the surface) would rust when exposed to oxygen and give those streaks of brown iron oxide.