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Several frequent approaches for inferring P-T route segments are: Mineral inclusions Some minerals contain inclusions

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For a few rocks, the only real part of the P-T path recorded during the mineral assemblage and texture from the rock could be the get more info 'peak' of metamorphism -- the conditions of your thermal highest (i.e., the utmost temperature along with the strain at the utmost temperature). When the rock experienced a sedimentary or volcanic protolith, it is possible to infer the rock started in the surface, arrived at peak problems at some temperature and depth within the Earth, and returned into the floor (wherever the rock was collected).

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As a result, The form of The trail, coupled with time data, delivers information regarding the driving forces

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