Explanation:

- Oxides: Comprise minerals formed by the combination of oxygen with metals. Not abundant enough to dominate the Earth's crust.

- Silicates: These minerals are formed from silicon and oxygen and make up more than 90% of the Earth's crust. They include familiar minerals like quartz, feldspar, and mica.

- Carbonates: Comprised of carbonate ion CO3, these minerals are significant in sedimentary rocks but don't dominate overall crustal composition.

- Sulphides and Sulphates: Composed of sulfur combined with metals or sulfate ion SO4, these minerals are present in the crust but are not the major constituents.