Metamorphic changes in the bulk composition of a rock primarily occur due to processes such as recrystallization, foliation, and the introduction of fluids. During metamorphism, existing minerals may alter into new minerals stable under the increased temperature and pressure conditions, often resulting in new mineral assemblages. The presence of fluids can facilitate ion migration, leading to changes in the rock's chemical composition and texture. Additionally, tectonic forces can induce stress, causing deformation and alignment of minerals, which further contributes to the metamorphic transformation.
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