1)Recrystallization: minerals change size and shape without changing the identity of the mineral.
2)Phase Change: transformation of one mineral to another mineral with the same composition, but different crystal structure.
3)metamorphic reaction: growth of new mineral crystals that differ from those of the protolith.
4)Pressure solution: in water, mineral grains partially dissolve because pressure is exerted unevenly on crystall surface.
5)Plastic deformation: rock is squeezed or sheered at high temperature. |