Highly fractionatedⅠ-type granites in NE China(Ⅱ):isotopic geochemistry and implications for crustal growth in the Phanerozoic
作者单位：InstituteofEarthSciencesAcademiaSinicaP.B.Box1-55NankangTaipei115TaiwanROC DepartmentofAppliedGeologyCurtinUniversityofTechnologyPerthWesternAustralia6845Australia DepartmentofGeologyNationalTaiwanUniversity245ChoushanRoadTaipei10770TaiwanROC GeosciencesRennes(CNRS)UniversitedeRennesIAvenueduGeneralLeclerc35042RennescedexFrance
会议名称：《中国科学院地质与地球物理研究所2003学术年会》
会议日期：2003年
学科分类：070902[理学-地球化学] 0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学]
摘 要：NE China is the easternmost part of the Central Asian Oogenic Belt(CAOB).The area is distinguished by widespread occurrence of Phanerozoic granitic *** the companion paper(PartⅠ),we establishe