%0 Journal Article
%T MINERALOGICAL CHARACTERISTICS-OF PHLOGOPITE-AMPHIBOLE-PYROXENITE MANTLE XENOLITHS INCLUDED IN THE ALKALI MAFIC-ULTRAMAFIC SUBVOLCANIC COMPLEX FROM LANGAO COUNTY,CHINA<br>岚皋碱性镁铁-超镁铁质潜火山杂岩中金云角闪辉石岩类地幔捕虏体矿物学特征
%A Huang Yuehua
%A <br>黄月华
%J 岩石学报
%D 1993
%I 
%X The phlogopite-amphibole-pyroxenite mantle xenoliths, occurring in early Palaeozoic alkali mafic-ultramafic subvolcanic complex in Langao County on the northern margin of Yangtze Plate, are composed of clinopyroxene, amphibole, phlogopite, apatite and illmenite. The rocks of xenoliths usually have coarse-fine granulitic, slab-granulitic, triplepoints, cataclastic and kink band textures with strongly developed the metasomatic textures. The studies on the characteristics of rocks and of mineral compositions show that the phlogopite-amphibole-pyroxenite xenoliths are the product of mantle metasomatism and they possibly represent the source of alkali mafic-ultramafic subvolcanic complex in this area.
%K Phlogopite-amphibole-pyroxenite Mantle Xenoliths
%K Mantle Metasomatism
%K Yangtze Plate
%K Langao County<br>金云角闪辉石岩
%K 地幔捕虏体
%K 地幔交代作用
%K 扬子板块
%K 岚皋
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=14A2F5715D4FB67FB5D4304C9A7699B9&yid=D418FDC97F7C2EBA&vid=9CF7A0430CBB2DFD&iid=E158A972A605785F&journal_id=1000-0569&journal_name=岩石学报&referenced_num=6&reference_num=0