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This is because of the differing densities of the two types of plate.

Oceanic plates are composed of mafic rocks which have higher concentrations of iron and magnesium than the silica and aluminum rich rocks of the crustal plates.

This concentration of iron and magnesium makes the oceanic crust more dense than the continental crust and so the oceanic crust tends to be forced under the continental crust at a subduction zone.

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