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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.
Regional Metamorphism. Metamorphism on a grander scale, called regional metamorphism, accompanies mountain-building activity. These metamorphic rocks pervade regions that have been subjected to intense pressures and temperatures during the development of mountain chains along boundaries between crustal plates.etamorphism that occurs in the course of increasing temperatures is called progressive. It is accompanied by the loss of volatile components (dehydration, decarbonatization) by the initial rocks. The opposite processes against a background of decreasing temperature are termed regressive metamorphism.