%0 Journal Article
%T A debate on the special circumstance of rock-forming and ore-forming of Haladala pluton, a mafic-ultramafic complex related to CuNi-VTiFe composite mineralization, in western Tianshan<br>西天山CuNi-VTiFe复合型矿化镁铁-超镁铁杂岩 ——哈拉达拉岩体成岩成矿背景特殊性讨论
%A Long Lingli
%A Wang YuWang
%A Tang PingZhi
%A Wang LiJuan
%A Wang JingBin
%A Liao Zhen
%A <br>龙灵利
%A 王玉往
%A 唐萍芝
%A 王莉娟
%A 王京彬
%A 廖震
%J 岩石学报
%D 2012
%I 
%X Haladala pluton,a mafic-ultramafic complex related to CuNi-VTiFe composite mineralization in western Tianshan,consists of troctolite,olivine gabbro,hornblende gabbro and diabase.The SHRIMP zircon U-Pb age of 308.8±1.9Ma,307.3±8.2Ma for olivine gabbro and gabbro of the Pluton were obtained.The major rock types in the Haladala pluton show cumulate texture,gabbro-ophitic textures,and the pluton exhibits well-developed rhythmic layering.All the different types rock of the plutons have rather similar trace-element distribution and REE patterns with positive Eu,Sr abnormity mostly,and it suggests they were the results of crystallization differentiation of the similar or same magma.The geochemical characteristics of Sr-Nd isotope compsition,initial 87Sr/86Sr values=0.703913～0.705259,εNd(t)=4.00～8.42,show that the original magma came from depleted mantle source.The study proposes that the Haladala pluton was formed in an early post-collisional orogenic stage,overlaying the possible mantle plume in the same time.
%K CuNi-VTiFe composite mineralization
%K Zircon U-Pb age
%K Sr-Nd isotope
%K Haladala
%K Western Tianshan
%K Xinjiang<br>CuNi-VTiFe复合型矿化
%K 锆石U-Pb年龄
%K Sr-Nd同位素
%K 哈拉达拉
%K 西天山
%K 新疆
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=6795DA99A00CC6A7857804D89BB578D2&yid=99E9153A83D4CB11&vid=D3E34374A0D77D7F&iid=DF92D298D3FF1E6E&sid=FFD10F7019FAA9EC&eid=DE9F9A03FB2549EC&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=53