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The two main families of rock-forming minerals are silicates and non-silicates. Silicates, which include minerals like quartz and feldspar, are the most abundant group and contain silicon and oxygen in their structure. Non-silicates, such as carbonates, oxides, and sulfates, do not include silicon and oxygen in their basic composition and comprise a diverse range of minerals. Together, these families contribute to the formation of igneous, sedimentary, and metamorphic rocks.

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