The Basic Principles Of 台北硬碟救援

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For a few rocks, the sole Component of the P-T path recorded during the mineral assemblage and texture of the rock is definitely the 'peak' of metamorphism -- the ailments in the thermal optimum (i.e., the most temperature along with the force at the maximum temperature). When the rock had a sedimentary or volcanic protolith, it is possible to infer which the rock started out in the area, arrived at peak problems at some temperature and depth inside the Earth, and returned to the area (where by the rock was gathered).

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