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The increasing garnets surrounded these relict minerals as the garnets grew, along with the relict minerals are preserved as mineralogical proof of an earlier stage in the metamorphic heritage from the rock.

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of other minerals. One example is, garnets usually consist of inclusions of minerals which were present within the rock matrix as the garnet grew, but which were not absolutely eradicated by metamorphic reactions in the course of progressive metamorphism.

P-T route condition by alone won't give a one of read more a kind interpretation of tectonic process or metamorphic driving forces. For example, clockwise paths can type in continental collision belts of subduction zones. Equally, some subduction zone rocks history clockwise paths and a few file counterclockwise paths. However, The combination of P-T path traits, time/fee information and facts, structural information, and various petrologic information and facts can offer important specifics of metamorphic and tectonic procedures.

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