Different minerals do melt and crystallize at different temperatures, showcasing partial melting and fractional crystallization, explained through Bowen's Reaction Series.
True. Different minerals indeed melt and crystallize at different temperatures. For example, quartz melts at a lower temperature compared to olivine.
As a rock heats up, the minerals that melt at the lowest temperatures will melt first, demonstrating partial melting. Fractional crystallization occurs during magma cooling, where different minerals crystallize at varying temperatures.
Bowen's Reaction Series explains the sequence in which minerals crystallize from magma, essential for understanding igneous petrology.
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