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of other minerals. By way of example, garnets normally have inclusions of minerals that were present in the rock matrix since the garnet grew, but that were not totally removed by metamorphic reactions in the course of progressive metamorphism.

P-T route shape by by itself isn't going to provide a unique Click Here interpretation of tectonic method or metamorphic driving forces. One example is, clockwise paths can variety in continental collision belts of subduction zones. Similarly, some subduction zone rocks record clockwise paths and a few record counterclockwise paths. Having said that, The combination of P-T path attributes, time/amount data, structural information, as well as other petrologic info can provide important specifics of metamorphic and tectonic procedures.

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