周振华;吕林素;王挨顺;

• 1:中国地质科学院矿产资源研究所国土资源部成矿作用与资源评价重点实验室
• 2:中国地质博物馆
• 3:内蒙古自治区地质调查院

摘要(Abstract)：

黄岗锡铁矿是大兴安岭南段成矿带的一个重要矿床,其广泛分布的花岗岩类与成矿有密切的成因联系。采用热电离质谱仪和LA-ICP-MS系统研究了黄岗花岗岩的Sr、Nd、Pb和Hf同位素组成特征,结果显示其[N(87Sr)/N(86Sr)]i值在0.702 11～0.707 29间,接近现代大洋玄武岩而小于大陆地壳的[N(87Sr)/N(86Sr)]i值,εNd(t)值在-0.8～0.9间,Nd模式年龄TDM介于993～855Ma间;Pb同位素值较高,N(206Pb)/N(204Pb)介于18.974～26.107间,N(207Pb)/N(204Pb)介于15.554～15.914间,N(208Pb)/N(204Pb)主要在38.894～39.890间,铅具有混合来源特征;N(176 Hf)/N(177 Hf)比值介于0.282 744～0.282 922间,εHf(t)值变化范围较大,为1.9～18.3,两阶段Hf模式年龄(TDM2)变化范围为888～561Ma。同位素组成特征表明,黄岗花岗岩的源区为起源于亏损地幔的初生下地壳物质的部分熔融,可能存在少量古老陆壳物质的混染。年轻的Nd、Hf同位素模式年龄暗示本区新元古代时期曾发生一次重要的地壳增生事件。结合区域晚中生代构造背景,黄岗花岗岩的形成机制为:被俯冲洋壳析出流体交代的地幔楔或亏损地幔减压部分熔融作用形成的基性岩浆分离后,诱发岩石圈拆沉、幔源岩浆上涌和底侵,促使镁铁质的初生地壳物质重熔并不断分异演化,从而产生了大量花岗岩浆,其地球动力学背景可能与太平洋板块的NNW斜向俯冲作用有关。

关键词(KeyWords)： 同位素地球化学;物质源区;岩石圈拆沉;太平洋板块;黄岗锡铁矿床

Abstract:

Keywords:

基金项目(Foundation): 中国地质调查局地质调查项目(1212010010923);; 中央级公益性科研院所基本科研业务费项目(K0921);; 内蒙古重要矿产资源潜力评价及区域成矿规律研究项目(2006-02-YS01);; 中国地质大学(北京)2008年度优秀博士论文扶持奖励基金项目

作者(Author): 周振华;吕林素;王挨顺;

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