台北硬碟救援 - An Overview

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For many rocks, the only Component of the P-T path recorded inside the mineral assemblage and texture of your rock would be the 'peak' of metamorphism -- the problems with the thermal greatest (i.e., the most temperature as well as the force at the utmost temperature). In case the rock experienced a sedimentary or volcanic protolith, you are able to infer that the rock started on the floor, arrived at peak circumstances at some temperature and depth while in the Earth, and returned into the surface (the place the rock was gathered).

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