Final answer:
The six common non-silicate mineral groups are carbonates, sulfates, sulfides, halides, oxides, and native elements. These minerals have different chemical compositions and can be found in various geological settings.
Step-by-step explanation:
The six common non-silicate mineral groups are carbonates, sulfates, sulfides, halides, oxides, and native elements.
Carbonates: These minerals contain the carbonate ion (CO3)-2 and are commonly found in sedimentary rocks. Examples include calcite and dolomite.
Sulfates: These minerals contain the sulfate ion (SO4)-2 and are often found in evaporite deposits. Gypsum and barite are examples of sulfates.
Sulfides: These minerals contain sulfur combined with a metal. Pyrite and galena are examples of sulfides.
Halides: These minerals contain a halogen ion (fluoride, chloride, bromide, or iodide). Halite (rock salt) and fluorite are examples of halides.
Oxides: These minerals contain oxygen combined with a metal. Hematite and magnetite are examples of oxides.
Native elements: These minerals contain a single element. Examples include gold, silver, and diamonds.