摘要
Shahre-BabakophioliteisapartoftheinnerZagrosophiolitebeltinIran.MajorpartsofintrusivemassesofShare-Babakophiolitearegabbroandplagiogranite.TheSiO2versusNa2O+K2Odiagramshowsthatthepalgiogranitesarerelatedtocalk-alkalineseries.Rareearthelementsexhibitrelativelysimilarpatternthatindicatestheserocksaresyngenetic.Also,REEpatternsdisplayanenrichmentofLREEcomparedtoHREE,andarecharacterizedbyflattoslightlyconcaveuppatternsfromGdtoYb.Suchpatternscontrastsharplywiththoseofplagiogranitesinmorecompleteophiolitesequences,suchastheSemailophiolite,Oman,ortheTroodosophiolite,Cyprus,andNeyriz,wherepatternsaremuchflatterandslightlyLREE-depleted.TheslightlyLREE-enrichedpatternsoftheShahre-Babakplagiogranitessupportapartialmeltingoriginforthem.ThelowTiO2,Nb,TacontentandhighLREEconcentrationsoftheShahre-Babakplagiogranitesindicatethattherockswerelikelyderivedfromtheanatexisofamphibolites,whichwererelatedtohydrothermalalterationofgabbrosinintra-oceanicback-arcbasin.
出版日期
2016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)