台中硬碟救援 - An Overview

Despite the fact that it is probably not doable to find out the trajectory in the P-T path from inclusions alone, inclusions can be made use of with other chemical and textural facts to higher define the path.

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For some rocks, the only real Component of the P-T path recorded within the mineral assemblage and texture of the rock is definitely the 'peak' of metamorphism -- the problems in the thermal optimum (i.e., the most temperature plus the strain at the maximum temperature). If the rock experienced a sedimentary or volcanic protolith, it is possible to infer that the rock started for the surface area, reached peak disorders at some temperature and depth from the Earth, and returned for the surface (wherever the rock get more info was collected).

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