%0 Journal Article
%T Metapelites in the Himalayan orogenic belt and their protoliths<br>喜马拉雅造山带变泥质岩系及其地球化学特征
%A ZENG LingSen
%A LIANG FengHu
%A XU ZhiQin
%A QI XueXiang
%A <br>曾令森
%A 梁凤华
%A 许志琴
%A 戚学祥
%J 岩石学报
%D 2008
%I 
%X Metapelites from the High Himalayan Crystalline Sequence (HHCS) and the North Himalaya Gneiss Dome (NHGD) have experienced upper amphibolite to granulite facies metamorphism.They consist dominantly of Al-rich gneiss with subordinate K- rich granitic gneiss,marble,and mafic granulite.Major and trace element data on a suite of the Himalayan metapelite show that (1) they are enriched in LILE and LREE relative to HFSE and HREE,respectively;(2) they have high contents of total REE,and substantial negative Eu ano...
%K Metapelite
%K Khondalite
%K Greater Himalaya
%K Tethyan Himalaya<br>变泥质岩
%K 孔兹岩系
%K 高喜马拉雅
%K 特提斯喜马拉雅
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=0DC31E264431712A1BC36330ACADB9CF&yid=67289AFF6305E306&vid=B91E8C6D6FE990DB&iid=DF92D298D3FF1E6E&journal_id=1000-0569&journal_name=岩石学报&referenced_num=6&reference_num=54