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The period of the path from start out (onset of metamorphism) to complete (publicity in the rock on the Earth's floor) will vary from rock to rock with regards to the tectonic background
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Factor zoning Metamorphic (and igneous) minerals may perhaps change composition in response to altering chemical and Bodily problems, for instance variations in stress-temperature situations, deformation variables, or chemical variables (e.g., existence of fluids). The chemical reaction of the mineral to those changes may be recorded in minerals that have crystal chemical and structural traits that enable compositions acquired early while in the mineral's expansion record to be preserved during later stages of development at distinct problems.
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