Pelitic, calcareous, felsic, and mafic refer to the chemical composition of this general class, but the actual number of minerals they contain is limited by the laws of thermodynamics.
Ulrich Grubenmann divided their zones of formation into the epizone, mesozone, and katazone, while Theodor Kjerulf and Karl Rosenbusch made key discoveries about them. Pelitic, calcareous, felsic, and mafic refer to the chemical composition of this general class, but the actual number of minerals they contain is limited by the laws of thermodynamics. They can also be classified structurally into mylonites, cataclastites, hornfels, gneiss, and schist. For 10 points, name this classification of rocks which, due to intense pressure or temperature, transform.
Ulrich Grubenmann divided their zones of formation into the epizone, mesozone, and katazone, while Theodor Kjerulf and Karl Rosenbusch made key discoveries about them.
{metamorphic} rocks