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For many rocks, the only Section of the P-T route recorded while in the mineral assemblage and texture of your rock may be the 'peak' of metamorphism -- the problems of your thermal maximum (i.e., the maximum temperature along with the tension at the maximum temperature). In case the rock experienced a sedimentary or volcanic protolith, you are able to infer the rock started off with the area, attained peak ailments at some Click This Link temperature and depth during the Earth, and returned on the area (where the rock was collected).
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Element zoning Metamorphic (and igneous) minerals may perhaps adjust composition in response to shifting chemical and physical disorders, for example modifications in force-temperature circumstances, deformation variables, or chemical things (e.g., existence of fluids). The chemical response of the mineral to these variations could possibly be recorded in minerals that have crystal chemical and structural attributes that allow compositions obtained early during the mineral's expansion history being preserved throughout afterwards stages of advancement at various ailments.
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