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- "u3010u200bu2029ufeffufe6au275bU000e013bufe37u24d4u002du1806u256au1806u247cu0085u17ac",
For many rocks, the one Element of the P-T route recorded within the mineral assemblage and texture of the rock would be the 'peak' of metamorphism -- the problems in the thermal optimum (i.e., the most temperature plus the strain at the maximum temperature). In case the rock experienced a sedimentary or volcanic protolith, you'll be able to infer that the rock begun with the area, reached peak disorders at Clicking Here some temperature and depth from the Earth, and returned for the surface (where by the rock was gathered).
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in comparison to the situations of the height of metamorphism stand for disequilibrium. Usually, however, the evidence for disequilibrium can be quite helpful because it can be utilized to reconstruct P-T route segments.