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CH3041
SILICATES II
• Extra cations give charge neutrality.
• eg. orthoclase feldspar KAlSi3O8
Al occupies 1 in every 4 tetrahedral sites,
the -ve charge is neutralised by the K+ 
•The bonding in the SiO44- tetrahedra has significant covalent character. 
• When a mineral dissolves the Si-O linkages are much stronger than the ionic cation-anion interactions and will break last.
Polymeric Silicates
Connection of the SiO4 tetrahedra may occur through 1 - 4 of the oxygen atoms.