%0 Journal Article
%T REE characteristics of Cu-Ni sulfide deposits in the Hami area, Xinjiang<br>新疆哈密黄山地区铜镍硫化物矿床的稀土元素特征及意义
%A WANG YuWang
%A WANG JingBin
%A WANG Lijuan
%A FANG TongHuiBeijing Institute of Geology for Mineral Resources
%A Beijing
%A ChinaKey Laboratory of Mineral Resources Research
%A Institute of Geology
%A Geophysics
%A Chinese Academy of Sciences
%A Beijing
%A China
%A <br>王玉往
%A 王京彬
%A 王莉娟
%A 方同辉
%J 岩石学报
%D 2004
%I 
%X On the base of study on the REE geochemistry of ore minerals and host rocks of typical deposits from Huangshan Cu-Ni metallogenic belt, Xinjiang, it was discovered that the host mafic-ultramafic rocks of the Cu-Ni sulfide deposits occurred in orogen are characterized by water-richment. Some REE pattern of sulfides shows particular " triplex curve" model, which suggests that due to coexistence of multiple liquid phase ( fluid and melt) , the sulfide melt possibly contained a lot of hydrothermal fluid and increasingly derived to gas and liquid-rich ore-forming fluid after the master metallogenic epoch (magmatic segregation stage). REE characteristics of the deposits in this area are quite different from thos of the Cu-Ni deposit occurred in cratonic margin, and the reason of hydrothermal fluid joining in mineralization might be owing to water-rich of ore-bearing rockbody that related to delamination and melting of water-rich oceanic crust in post-collision stage.
%K Cu-Ni sulfide deposit
%K "Triplex curve" model of rare earth elements
%K Water-rich mafic-ultramafic rock
%K Xinjiang<br>铜镍硫化物矿床
%K 稀土元素的“三重弯曲”模式
%K 富水镁铁-超镁铁岩
%K 新疆
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=86C06DB5CBBDD650&yid=D0E58B75BFD8E51C&vid=A04140E723CB732E&iid=E158A972A605785F&sid=073C3CF5F13F64FE&eid=29C36F017AD88B64&journal_id=1000-0569&journal_name=岩石学报&referenced_num=18&reference_num=72