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For that reason, While subduction zone rocks can observe several paths through subduction and exhumation, analyzing the precise route that a certain exhumed subduction zone rock adopted is vital for comprehension subduction dynamics.

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For many rocks, the sole Portion of the P-T route recorded in the mineral assemblage and texture on the rock will be the 'peak' of metamorphism -- the ailments from the 台北硬碟救援 thermal most (i.e., the utmost temperature and also the tension at the most temperature). If your rock experienced a sedimentary or volcanic protolith, you'll be able to infer the rock began in the surface, reached peak situations at some temperature and depth from the Earth, and returned to the surface (exactly where the rock was gathered).

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