GEOCHEMISTRY OF EARLY CRETACEOUS TRACHYTES OF DONGLINGTAI FORMATION FROM THE XISHAN AREA, BEIJING: CONSTRAINTS ON MELTING OF LOWER MAFIC CRUST

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摘要 TheearlyCretaceoustrachytesofDonglingtaiFormationinXishan,BeijingarecharacterizedbyslightEunegativeanomalyandsignificantenrichmentinLREE,LILE(Ba,KandSr)anddepletionofNb-Ta-Ti,Th-U.ThesetrachyteshavebeenhighlyenrichedbySrandNdisotopicsignatures(87Sr/86Sr(t)=0.70638~0.70672,εNd(t)=-16.3~-15.7),overlappingSr-NdisotopicrangeoflateMesozoicmaficigneousrocksintheregion.TakingintoaccountNb-TafractionationandhighZr/Smratioforthesetrachytes,weconsiderthatthetrachytesofDonglingtaiFormationarederivedfromthegarnet-bearingamphiboliteinthelowercrustcomposedofgarnet+plagioclase±amphibole±pyroxeneresidualphases.OnthebasisofthemeltingexperimentalresultsofcrustalmaterialsandregionalextensionaltectonicsduringlateMesozoic,itisconcludedthatthethermalinputfromunderplatingbasalticmeltresultsinthepartialmeltingoflowercontinentalcrusttogeneratethetrachytesofDonglingtaiFormation.AndthecharacteristicsofhighSrandBaforthesetrachytessuggestthatpartofunderplatingbasaltsshouldtakeashareinpartialmeltingatleast.
机构地区 不详
出版日期 2005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)
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