%0 Journal Article
%T Eclogite facies garnet-pyroxenolite xenolith in Hannuoba area: New evidence of magma underplating<br>汉诺坝榴辉岩相石榴辉石岩——岩浆底侵作用新证据
%A FAN QiCheng
%A SUI Jianli
%A LIU RuoXin
%A ZHOU Xinmin
%A <br>樊祺诚
%A 隋建立
%A 刘若新
%A 周新民
%J 岩石学报
%D 2001
%I 
%X Eclogite facies garnet pyroxenolite xenoliths in Hannuoba area show the typical layered cumulate structures and crystalloblastic textures of granulite facies. The mineral compositions, equilibrated P T conditions and REE geochemistry of the xnolith reveal its mantle derived genesis. All these facts indicate that the mantle derived magma underplates in the top of the upper mantle and forms the mafic cumulate, then the cumulate experiences some metamorphism of eclogite facies. The eclogite facies xenolith, accomponied with the granulite facies xenolith, provides new evidence of the existence of the crust mantle transitional zone.
%K Eclogite facies garnet-pyroxenolite xenoliths
%K Magma underplating
%K Crust-mantle transitional zone
%K Hannuoba area<br>岩浆底侵作用
%K 壳－幅过渡带
%K 榴辉岩相石榴辉石岩捕虏体
%K 产状
%K 层状堆晶构造
%K 岩石学
%K REE地球化学
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=53A1058B6EE454EC&yid=14E7EF987E4155E6&vid=BCA2697F357F2001&iid=CA4FD0336C81A37A&sid=CA4FD0336C81A37A&eid=B31275AF3241DB2D&journal_id=1000-0569&journal_name=岩石学报&referenced_num=43&reference_num=29