Generally referred to as micaceous minerals, biotite and muscovite are silicate minerals having perfect basal cleavage. They both contain most of the same elements, just in different quantities. However, biotite is soluble in sulfuric acid and has iron and magnesium in it, where muscovite does not. They can be found in all types of rock.
Chemical composition determines density. In this case, I think it's safe to implicate iron content.
Slate is mainly composed of the minerals quartz and muscovite or illite
The majority of minerals associated with igneous rocks are silicates. It is the proportion of certain silicate minerals that affects the color of igneous rocks. Igneous rocks that are high in orthoclase feldspar, quartz, and muscovite mica will be lighter in color than igneous rocks that are higher in olivine, pyroxene, amphibole, and biotite mica.
granite
Muscovite generally displays a micaceous crystal habit, of thin flexible sheets.
Biotite mica contains iron and/or magnesium, but muscovite mica does not.
Both are platy, silicate, mica group minerals with perfect cleavage in one direction.
Biotite and Muscovite.
Quartz, Feldspar, Muscovite, Biotite are among most common silicate minerals.
Platy minerals are micas(muscovite and biotite) and chlorite
Mica is a group of sheet silicate minerals (e.x of micas : Biotite, muscovite)
Mica minerals have only one direction of cleavage. Examples are Muscovite and Biotite.
Biotite mica contains iron and/or magnesium, but muscovite mica does not.
Muscovite (clear) and Biotite (black) are the commonest mica forms. Fuchsite (green) is an unusual mica containing chromium. Please see the related link below for a listing of the mica group of minerals.
micas such as muscovite, biotite
Many minerals separate into sheets. If the mineral has cleavage than it is common for it to separate into sheets. Mica separates into sheets.
There are ten minerals that are so common that they make up 90% of the Earth's crust. These are quartz, orthoclase, plagioclase, muscovite, biotite, calcite, dolomite, halite, gypsum, and ferromagnesian minerals.