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of a metamorphic rock will be the list of all P-T ailments expert by a rock for the duration of its metamorphic historical past (Figure 1).
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paths The idealized see of P-T paths is the fact mineral assemblages equilibrate at every phase of The trail in the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This look at ignores kinetic things linked to the energetics of nucleation and advancement of minerals, Even though these variables could possibly be essential for some metamorphic phases and reactions. For instance, the Discover More presence of coexisting andalusite and sillimanite (Fig. 6a) in a very rock that equilibrated at P-T conditions similar to The soundness subject of sillimanite illustrates the sluggish kinetics from the andalusite-to-sillimanite transformation allowed andalusite to persist metastably outside its balance industry. It's important to acknowledge the affect of deformation on metamorphic reactions, along with the extent to which deformation (pressure Strength) might guide reactions.
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