(1) Institute of Geology, Chinese Academy of Geosciences, 100037 Beijing, China;(2) Open Laboratory of Changchun Geological College, 130021 Changchun, China
Abstract:
HighP-T experiment with natural massive rock sample of garnet biotite plagioclase gneiss indicates that the metamorphic reaction involving melt (reaction between relic mineral phase and melt) is the most important reaction in granulite-facies metamorphism and accompanies anatexis process.