Phase equilibria in metamorphic rocks. Thermodynamic background and petrological applications / Фазовые равновесия в метаморфических породах. Термодинамические предпосылки и петрологические приложения

Metamorphic rocks make up much of the deeper parts of orogenic belts. The minerals and mineral assemblages present in these rocks contain information about the conditions of formation of the rocks. This information may be used to decipher parts of the tectonometamorphic processes that were involved in the formation of the rocks. The unravelling of the conditions of formation is therefore important if the tectonothermal history of an orogen is to be determined <...>