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The escalating garnets surrounded these relict minerals since the garnets grew, and the relict minerals are preserved as mineralogical proof of an previously phase while in the metamorphic history on the rock.

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paths The idealized look at of P-T paths is the fact mineral assemblages equilibrate at every stage of the path through the onset of metamorphism to the height of metamorphism, at which the ultimate assemblage is locked in. This perspective ignores kinetic factors relevant to the energetics of nucleation and advancement of minerals, Though these components may very well be significant for some metamorphic phases and reactions. For example, the existence of coexisting andalusite and sillimanite (Fig. 6a) within a rock that equilibrated at P-T situations equivalent to The steadiness area of sillimanite illustrates which the sluggish kinetics with the andalusite-to-sillimanite transformation permitted andalusite to persist metastably outside its steadiness subject. It Discover More Here is vital to recognize the impact of deformation on metamorphic reactions, as well as the extent to which deformation (strain Electricity) may possibly help reactions.

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