I too would like an answer to this question as it seems hornfels
could be of varying grade dependant on the temperature. The facies
of contact metamorphism progress in temperature at relatively low
pressure from the Albite-Epidote Hornfels Facies to the Hornblende
Hornfels Facies, to the Pyroxene Hornfels Facies.
It seems that hornfels do have differant grades.