Abstract
Metamorphic processes are closely associated with the formation and evolution of the crust and strongly related to petrogenetic and mineralization processes. Fluid inclusions analyses indicate that regional metamorphic migmatization and anatexis are temperature-pressure progressive processes. Metamorphic anatexis is an ultra-metamorphic process at higher temperature and higher pressure than the migmatization process. It is characterized by high temperature and pressure (HP-HT) fields, metasomatism-melting and spatio-temporal distribution.
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