Monazite is considered a diagnostic accessory mineral of s type granites whereas allanite is diagnostic of i type granites.
Minerals in granite include.
Color variation is a response to the percent of each mineral found in the sample.
Accessory minerals commonly observed in s type granites include zircon apatite tourmaline monazite and xenotime.
Oxide minerals in s type granites will more commonly be ilmenite rather than magnetite.
It also contains some mafic minerals mainly biotite and amphibole all black and other dark colored minerals.
A granitoid a coarse grained igneous rock composed mostly of quartz k feldspar alkali feldspar and plagioclase.
Granite is high in quartz about 25 feldspar and mica.
The sodic amphiboles and pyroxenes riebeckite arfvedsonite aegirine are characteristic of the alkali granites.
More specifically a rock having an alkali feldspar total feldspar ratio from 0 35 0 90 on the qapf diagram and 20 60 quartz.
The crystals in granite provide a variety of mixed colors feldspar pink or red mica dark brown or black quartz clear pink white or black and amphibole black.
If neither feldspar is in great excess neither amphibole nor pyroxene is likely to be an essential constituent.
Granite is composed mainly of quartz and feldspar with minor amounts of mica amphiboles and other minerals.
The minor essential minerals of granite may include muscovite biotite amphibole or pyroxene.
This mineral composition usually gives granite a red pink gray or white color with dark mineral grains visible throughout the rock.
Granite is composed of varying amounts of the must have minerals quartz potassium feldspar orthoclase feldspar penis sanidine feldspar microcline feldspar plagioclase feldspar and may but.
Pyroxene is rarely present.
Granite mainly consists of felsic minerals namely alkali feldspar all the pink colored minerals you see in granite plagioclase and quartz all the white and light gray colored minerals.