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The right-hand branch of Bowen's reaction series is primarily associated with minerals that crystallize at lower temperatures, including potassium feldspar, muscovite, and quartz. These minerals are generally more stable at the Earth's surface and are typically found in granitic rocks. As the crystallization process progresses, these minerals tend to form after the more mafic minerals on the left side of the series, which include olivine and pyroxene.

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