摘要
ThespinelperidotitexenolithsofGroupIinQuaternarybasanitesfromNushan,Anhuiprovince,canbeclassifiedastwosuites:ahydroussuitecharacterizedbytheubiquitousoccurrenceof(Ti-)pargasiteandananhydroussuite.Thenineralchemistryrevealsthattheanhydroussuiteandoneassociatedphlogopite-bearinglherzoliteareequilibratedundertemperatureconditionsof1000-1100℃,whereasamplhibole-bearingperidotitesdisplaydistinctdisequilibrumfeatures,indicatingpartialreequilibrationfrom1050to850℃andlocallydownto750℃.Theamplhbole-bearingperidotiteswereprobablytheuppermostpartofthehightemperatureanhydroussuitewhichwasmodallymodifedbyfractionatingH2O-richmetasomaticagentduringregionalupwelling.Thisrelativelyrecentlithosphericuplifteventfollowedanolderuplifteventrecognizedfrompyroxeneunmixingofdomainsinlocalequilibrium,aswellasthedominantdeformationtextureintheanhydroussuite.ThefirstthermaldisturbancecanbelinkedwiththeregionalextensionandwidespreadbasalticvolcanisminJiangsu-AnhuiprovincessinceEarlyTertiaryandtheformationofthenearbySubei(NorthJiangsu)fault-depressionbasinduringtheEocene,whilethesecondeventinassociationwiththeformationofamphibolesprobablyindicatesthecontinuationbutdiminutionofupwaredmantlefluxsinceNeogeneinresponsetothechangeintectonicregimeforeasternchina.
出版日期
1997年03月13日(中国期刊网平台首次上网日期,不代表论文的发表时间)