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Consequently, Whilst subduction zone rocks can follow numerous paths throughout subduction and exhumation, figuring out the specific path that a particular exhumed subduction zone rock followed is important for understanding subduction dynamics.

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The trajectory and shape of your P-T route, the charges of metamorphic processes, as well as length of metamorphism certainly are a function of your supply of heat and the mechanisms of burial and unroofing (if force modify is involved).

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paths The idealized perspective of P-T paths is the fact mineral assemblages equilibrate at Check Out Your URL every single phase of The trail within the onset of metamorphism to the peak of metamorphism, at which the ultimate assemblage is locked in. This look at ignores kinetic elements connected with the energetics of nucleation and growth of minerals, although these things can be significant for some metamorphic phases and reactions. For example, the presence of coexisting andalusite and sillimanite (Fig. 6a) in a rock that equilibrated at P-T conditions corresponding to The steadiness subject of sillimanite illustrates the sluggish kinetics from the andalusite-to-sillimanite transformation authorized andalusite to persist metastably exterior its security area. It is important to acknowledge the affect of deformation on metamorphic reactions, and the extent to which deformation (pressure Vitality) might guide reactions.

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