I type granites are a category of granites originating from igneous sources first proposed by chappell and white 1974.
Magma white granite.
Granite is formed by the cooling of magma in the ground.
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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Petrographic features are.
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.
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Granite is a light colored igneous rock with grains large enough to be visible with the unaided eye.
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