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Time plays a crucial role in the formation of metamorphic rocks as it allows for the gradual changes in temperature, pressure, and chemical processes that alter the original rock (parent rock). Over extended periods, these conditions facilitate recrystallization, foliation, and the development of new minerals, transforming the rock's structure and composition. The longer the time under these conditions, the more pronounced the metamorphic features become, ultimately leading to the creation of distinct metamorphic rock types.

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3mo ago

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