摘要
Unlikethemagmaintrusionmodel,thein-situmeltinghypothesisadvancedinthelastdecaderegardstheuppercrustasaclosedsystem,andgraniteastheresultofthematerialswithinsystemchangingfromorder(protolith)todisorder(melts)andtoneworder(granite)withthevariationsofentropyofthesystem.ThevariousgeologicalandgeochemicaldatafromtheMesozoicgranitesofsoutheastChinaareexplainedlogicallyandsystemicallybythehypothesis,concludingthattheyshouldbeoriginatedfromthemeltingofprotoliths.
出版日期
2001年01月11日(中国Betway体育网页登陆平台首次上网日期,不代表论文的发表时间)