台北硬碟救援 - An Overview

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For many rocks, the only part of the P-T path recorded during the mineral assemblage and texture on the rock is definitely the 'peak' of metamorphism -- the situations of your thermal optimum (i.e., the utmost temperature plus the pressure at the utmost temperature). Should the rock had a sedimentary or volcanic protolith, you could infer that the rock started with the area, reached peak problems at some temperature and depth during the Earth, and returned towards the surface (in which the rock was gathered).

P-T path form by alone does not supply a exclusive interpretation of tectonic approach or metamorphic driving forces. Such as, clockwise paths can form in continental collision belts of subduction zones. Likewise, some subduction zone rocks file clockwise paths and many history counterclockwise paths. Nevertheless, The combination of P-T route properties, time/rate info, structural info, together with other petrologic information can provide considerable information regarding metamorphic and tectonic procedures.

Thus, The form Click Here of The trail, coupled with time facts, delivers specifics of the driving forces

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