You think probable to manganese metasilicate Mn(SiO3)2.
silicate minerals and non silicate minerals
Heck to the no...
The simple answer is... Feldspar has a much higher complex and stable tetrahedral orientation in comparison to that of any other Silicate variation higher up on the reation series latter. Feldspar is one of the most stable variations in orientation of, what boils down to, silicate tetrahedra. Because Feldspar is technically a form of silicate tetrahedra orientation, I am assuming you are asking how the silicate tetrahedra orientations vary from its most simple (i.e. Olivine) to its mosts complex (i.e. quartz/FELDSPAR) forms. Esentially a Silicate Ion SiO4^-4 is the most basic building block of FELDSPAR. Knowing this, as you move from the top of Bowen's reaction series, we see a gradual stabilization of the various Silicate tetrahedral orientations. These orientations include (in order of stability/complexity): [TOP OF REACTION SERIES] Individual (Singular form) Silicate Tetrahedra (i.e. Olivine) Chain (Linear form) Silicate Tetrahedra (i.e. Pyroxine) Double Chain (Bilinear form) Silicate Tetrahedra (i.e. amphibole) Sheet Silicate Tetrahedra ('2-D' form) (i.e. Mica: Biotite or Muscovite) Framework Silicate Tetrahedra ('3-D' form) (i.e. FELDSPAR) [BOTTOM OF REACTION SERIES]
chicken
A stalagmite is a build up of silicate on the base of a cave, many times in the shape of a cone with the base on the floor of the cave, as it extends to the ceiling.
The chemical formula for Calcium Silicate is Ca2SiO4.
chemical formula for sodium silicate is Na2SiO3
The chemical formula of magnesium silicate is MgSiO3.
Sodium silicate is Na2SiO3
It is a non-silicate. Its chemical formula is CaF2.
Formula: FeSiO3
A silicate mineral contains silicon (Si) and oxygen (O) which will be shown in the formula.
Na2SiO3
CaSiO3
fezno2
CdSiO3
The formula is CaSiO4.