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The length of The trail from start (onset of metamorphism) to finish (exposure in the rock with the Earth's floor) will vary from rock to rock based on the tectonic background

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paths The idealized look at of P-T paths is mineral assemblages equilibrate at each stage of the path with the onset of metamorphism to the height of metamorphism, at which the final assemblage is locked in. This see ignores kinetic elements related to the energetics of nucleation and growth of minerals, While these elements may very well be crucial for some metamorphic phases and reactions. Such as, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T conditions similar to The steadiness discipline of sillimanite illustrates that the sluggish kinetics of your andalusite-to-sillimanite transformation Continue authorized andalusite to persist metastably outdoors its stability industry. It can be crucial to acknowledge the influence of deformation on metamorphic reactions, and the extent to which deformation (pressure Strength) could assist reactions.

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