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Pyroxenes are a group of rock-forming silicate minerals. They are comprised of single chains of silica tetrahedra and have the general formula XY(Si,Al)2O6.

X represents calcium, sodium, iron+2 and magnesium and more rarely zinc, manganese and lithium. Y represents ions of smaller size, such as chromium, aluminium, iron+3, magnesium, manganese, scandium, titanium, vanadium and even iron+2. Although aluminium commonly substitutes for silicon in other silicates, it usually doesn't substitute for silicon in a pyroxene.

The name pyroxene comes from the Greek words for fire and stranger. It was named that way due to their presence in volcanic lavas, where they are sometimes seen as crystals embedded in volcanic glass; it was assumed that were impurities in the glass, hence the name "fire strangers". However, they are simply early forming minerals that crystallized before the lava erupted.

The mantleThe mantle is the layer in the structure of the Earth that lies directly under the Earth's crust. It lies between 30 and 2,900 km below the surface. The boundary between the crust and the mantle is the Mohorovicic discontinuity, named for its discoverer, of Earth is composed mainly of olivineThe mineral olivine is a magnesium iron silicate with the formula (Mg,Fe)SiO in which the ratio of magnesium and iron varies between the two endmembers of the series: forsterite (Mg-rich) and fayalite (Fe-rich). It gives its name to the group of minerals and pyroxene.

Some pyroxenes:



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