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Regional metamorphism is metamorphism that occurs over broad areas of the crust. Most regionally metamorphosed rocks occur in areas that have undergone deformation during an orogenic event resulting in mountain belts that have since been eroded to expose the metamorphic rocks.
In order to get a schist, we need to have foliated rocks, which are due to a differential pressure. The most common cause of differential pressure is orogenesis or a mountain-building event. An orogeny occurs when plate tectonics cause the collision of 2+ plates.