Felsic rocks are light coloured, contain felsic minerals (e.g. qtz, feldspar, feldspathoids) which are themselves light in colour and have a low density which contribute to the pale colour of the rock.
Mafic Rocks are denser and dark coloured, the result of containing mafic minerals (pyroxene, amphibole, olivine, biotite). These minerals contribute to the green, brown and black colour of these rocks.
Ultramafic vs. ultrabasic
Used in reference to the SiO2 and Al2O3 which are the two most abundant components of igneous rocks.
Minerals present in igneous rocks can be divided into two groups:
Those which are compatible with quartz or primary SiO2 mineral (tridymite, cristobalite) these minerals are saturated with respect to Si, e.g feldspars, pyroxenes.
Those which never occur with a primary silica mineral. These are undersaturated minerals, e.g. Mg-rich olivine, nepheline.
The occurrence of quartz with an undersaturated mineral causes a reaction between the two minerals to form a saturated mineral.
2SiO2 + NaAlSiO4 ===> NaAlSi3O8
Qtz + Ne ===> Albite
SiO2 + Mg2SiO4 ===> 2MgSiO3
Qtz + Ol ===> En
Rock Classification (Silica saturation)
Oversaturated - contains primary silica mineral
Saturated - contains neither quartz nor an unsaturated mineral
Unsaturated - contains unsaturated minerals
Four subdivisions of rocks independant of silica saturation, based on the molecular proportions of Al2O3, Na2O, K2O and CaO applied mainly to granitic lithologies.