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The trajectory and condition of the P-T path, the costs of metamorphic procedures, and the length of metamorphism are a function in the supply of heat and the mechanisms of burial and unroofing (if force adjust is involved).
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Component zoning Metamorphic (and igneous) minerals could modify composition in reaction to changing chemical and physical situations, for example improvements in force-temperature disorders, deformation variables, or chemical things (e.g., existence of fluids). The chemical reaction of the mineral to those improvements may very well be recorded in minerals which have crystal chemical and structural attributes that permit compositions acquired early within the mineral's development Continued historical past for being preserved for the duration of later stages of growth at different circumstances.
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