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The property is their chemical formula.
silicate minerals and non silicate minerals
The grouping of silicate and non-silicate minerals is based on whether they contain silicon and oxygen. Silicate minerals are divided into smaller groups based on their structure. Non-silicate minerals are didvided into smaller groups based on their composition.
Neso-, soro-, cyclo-, ino-, phyllo- and tectosilicates are all the groups of silicate minerals.
nonsilicate and silicate minerals
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nonsilicate and silicate minerals
Quartz and feldspars are the most common silicate minerals of the crust.
silicate: feldspar and mica non-silicate: halides and native gold
Non-silicate mineral groups include: oxides, carbonates, sulfides, sulfates, borates, halites, elemental, organic, and phosphates.
Quartz is the most abundant single mineral. Feldspars are, as a group, the most abundant minerals. Quartz and feldspars are classified as silicate minerals, the classification of mineral with the most abundance in the Earth's crust.
Minerals can be classified into 13 groups according to their constituents. The major groups are: (1) native elements; (2) sulfides; (3) sulfosalts; (4) oxides and hydroxides; (5) halides and borates; (6) carbonates; (7) nitrates and iodates; (8) phosphates, vanadates, and arsenates; (9) sulfates; (10) tungstates and molybdates; and (11) silicates.