How does silicon occur in Earth’s mantle?

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In Earth’s mantle, silicon occurs primarily in combination with oxygen and other elements as silicate minerals. During the early geochemical differentiation of the planet, silicon—along with magnesium—exhibited a strong affinity for oxygen, leading it to combine completely with oxygen to form these compounds.12

The mantle is composed largely of magnesium-iron silicates, specifically olivine and pyroxene, or their high-pressure equivalents. These minerals serve as critical structural components of the mantle, distinguishing it from the crust, which is enriched in elements that do not readily enter the crystal structures of these specific silicate minerals.2