The chemical formula for micas varies, but they typically have the general formula:
(K,Na,Ba,Rb,Ca)(Al,Mg,Fe)2(Si3Al)O10(OH,F)2
Where:
- K, Na, Ba, Rb, and Ca represent alkali metals and alkaline earth metals that can occupy the interlayer sites. Potassium is the most common.
- Al and Mg represent aluminum and magnesium that occupy the octahedral sites between the silica tetrahedral sheets.
- Fe can substitute for Al in the octahedral sites.
- Si and Al occupy the tetrahedral sites within the silica sheets. The ratio of Si to Al is typically around 3:1.
- O represents oxygen atoms
- OH or F can occupy the interlayer sites, with hydroxyl (OH) being
- more common. Fluorine can substitute for hydroxyl in some micas.
So in summary, micas have a layered aluminosilicate structure with interlayer cations that can vary, but they are generally characterized by an approximate 3:1 ratio of silicon to aluminum within the silica tetrahedral sheets. The chemical formula given is the generalized structural formula for micas, but the actual compositions can vary based on the specific mica.