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In contact metamorphism - a nearby magma melt.

In regional metamorphism - the geothermal gradient from the mantle/core

In mylonites, the heat of friction across the fault plane.

In astroblemes, the kinetic energy of the impactor.

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The origin of the heat that creates metamorphic rock can be from friction caused by colliding plates, but by far the vast majority of the heat has originated in Earth's interior, caused by radioactive decay, remnant heat from Earth's formation, and pressure.

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15y ago

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