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+ //kOffsetContainsValue = 0x80000000 // Offset has value for father or mother node ; // The 2 node kinds are distinguished with the kVerticalNode flag.
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For many rocks, the only real Section of the P-T route recorded from the mineral assemblage and Continued texture on the rock may be the 'peak' of metamorphism -- the circumstances of the thermal utmost (i.e., the utmost temperature as well as the pressure at the most temperature). If your rock had a sedimentary or volcanic protolith, you are able to infer which the rock begun with the surface area, reached peak ailments at some temperature and depth inside the Earth, and returned towards the surface (in which the rock was gathered).
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