Experimental study of the metamorphic reaction involving melt under high temperature and high pressure  

作　　者：Fulai Liu Qihan Shen Yuansheng Geng Xuechun Xu Rui Ma 

机构地区：[1]Chinese Acad Geosci, Inst Geol, Beijing 100037, Peoples R China [2]Changchun Geol Coll, Open Lab, Changchun 130021, Peoples R China

出　　处：《Chinese Science Bulletin》1998年第3期249-253,共5页

基　　金："MetamorphicDynamicsOpenLaboratory"inChangchunGeologicalCollege;theFoundationofYouthGeologistofMinistryofGeologyandMineralResources (GrantNo .96 0 3)

摘　　要：High P_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.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.

关 键 词：METAMORPHIC reaction involving MELT natural massive rock GARNET BIOTITE PLAGIOCLASE GNEISS high_temperature and high_pressure experiment. 

分 类 号：P588.3[天文地球—岩石学]