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When magma forms by partial melting, the first minerals to melt are typically those with lower melting points, such as olivine and pyroxene. These minerals are rich in iron and magnesium and tend to crystallize at higher temperatures. As melting progresses, other minerals like amphibole and biotite may also begin to melt, contributing to the composition of the resulting magma. This selective melting is influenced by the mineral's chemistry and the temperature and pressure conditions present in the Earth's crust.

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