摘要
1IntroductionPetrogenesisofMesozoicgranitoidsinMongoliathatcomprisetheMongol-Okhotskfoldbeltwasstudiedduringmorethan40years.ThisbeltiswellknownprovinceoftheMesozoicmagmatismandmineralizationincludinggold,copperandmolybdenum,tinandtungsten,leadandzinc,andfluorite.Inthemiddleofthe1950'sChenGuodaproposedthediwatheorytoexplaintectonicactivityinChineseplatform.InRussianFarEastforsimilarprocessestheactivization(revivation)theorywasproposedwhichexplainedintracontinentaleventsintheMongol-okhotskfoldbwlt.
出版日期
2001年01月11日（中国期刊网平台首次上网日期，不代表论文的发表时间）
