%0 Journal Article
%T Features of the mantle source of the Huangshanxi Ni-Cu sulfide-bearing mafic-ultramafic intrusion, eastern Tianshan<br>东天山黄山西含铜镍矿镁铁-超镁铁岩体岩浆地幔源区特征研究
%A DENG YuFeng
%A SONG XieYan
%A CHEN LieMeng
%A CHENG SongLin
%A ZHANG XinLi
%A LI Jun
%A <br>邓宇峰
%A 宋谢炎
%A 陈列锰
%A 程松林
%A 张新利
%A 李军
%J 岩石学报
%D 2011
%I 
%X Huangshan-Jingerquan copper-nickel mineralization belt is located in Late Paleozoic eastern Tianshan orogenic belt, which is part of the Central Asian orogenic belt. This mineralization belt is the second largest copper-nickel deposit base in China other than the Jinchuan deposit, with total reserves of copper, nickel up to one million tons. The Huangshanxi Cu-Ni ore deposit is one of the large deposits in the Huangshan-Jingerquan copper-nickel mineralization belt. The average grade of copper is 0.31%, with...
%K Huangshan-Jingerquan Cu-Ni mineralization belt
%K Huangshanxi mafic-ultramafic intrusion
%K Magma Cu-Ni sulfide deposit
%K Metasomatized mantle
%K Asthenosphere<br>黄山-镜儿泉铜镍成矿带
%K 黄山西镁铁-超镁铁岩体
%K 岩浆铜镍矿床
%K 交代地幔
%K 软流圈
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=3897C9445ED3113AD4ACFA2331978985&yid=9377ED8094509821&vid=DB817633AA4F79B9&iid=59906B3B2830C2C5&sid=250CB55D2EF61CAC&eid=2A08EE1B5E82E505&journal_id=1000-0569&journal_name=岩石学报&referenced_num=3&reference_num=110