These are most common minerals *
5 points
atoms, crystals and compounds
muscovite, biotite and jasper
pyrite, olivine, dolomite
feldspar, quartz and silicates

Feldspar, quartz, and silicates

Explanation:

The most common mineral in the Earth's crust is feldspar, which accounts for somewhat less than two-thirds of the total. After feldspar, silicates would be the next most important, but the total percentage of silicates is not too much greater than that of quartz.

In total, almost ninety percent of the minerals found in the Lithosphere belong to one of these three groups of mineral. The situation naturally changes drastically if the Mantle and Core are considered.

periodic trends is an atom that gets larger as the number of electronic shells increase, the radius of atoms increases as you go down a certain group in the periodic table of elements. in general, the size of an atom will decrease as you move from left to right of a certain period.