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Regional metamorphism is a geological process that affects a wide area, involving mineralogical and structural adjustments in rocks due to conditions different from their original formation. This type of metamorphism typically occurs with a general increase in both temperature and pressure over a large region.12

Key aspects of regional metamorphism include:
* Agents of Change: Temperature, pressure, and fluids are the primary drivers.2
* Processes: It involves mechanical dislocation and chemical recrystallization, leading to new mineral assemblages.2
* Facets: The amphibolite facies is a common high-grade example, characterized by minerals like hornblende and plagioclase feldspar, often resulting in foliated or schistose rocks.3

Unlike contact metamorphism (driven by heat from intrusions) or dynamic metamorphism (driven by mechanical deformation), regional metamorphism encompasses broad geological areas.2

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