It forms from the slow crystallization of magma below earth s surface.
Magma white granite.
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They are recognized by a specific set of mineralogical geochemical textural and isotopic characteristics that indicate for example magma hybridization in the deep crust i type granites are saturated in silica but undersaturated in aluminum.
Petrographic features are.
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Granite is composed mainly of quartz and feldspar with minor amounts of mica amphiboles and other minerals this mineral composition usually gives granite a red pink gray or white color with dark mineral.
Granite is by far the most common rock found in the outer crust of the planet.
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