| 新疆北山地区两个含铜镍镁铁—超镁铁质岩体铂族元素地球化学研究 |
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| 引用本文： | 柴凤梅,夏芳,陈斌,卢鸿飞,王恒,李军,严玉圃.新疆北山地区两个含铜镍镁铁—超镁铁质岩体铂族元素地球化学研究[J].地质学报,2013,87(4):474-485. |
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| 作者姓名： | 柴凤梅 夏芳 陈斌 卢鸿飞 王恒 李军 严玉圃 |
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| 作者单位： | 新疆大学地质与矿业工程学院，新疆中亚造山带大陆动力学与成矿预测实验室，乌鲁木齐，830049；;新疆大学地质与矿业工程学院，新疆中亚造山带大陆动力学与成矿预测实验室，乌鲁木齐，830049；;新疆大学地质与矿业工程学院，新疆中亚造山带大陆动力学与成矿预测实验室，乌鲁木齐，830049；北京大学地球与空间科学学院，北京, 100871;新疆维吾尔自治区地质矿产勘查开发局第六地质大队，新疆哈密, 839000;新疆维吾尔自治区地质矿产勘查开发局第六地质大队，新疆哈密, 839000;新疆维吾尔自治区地质矿产勘查开发局第六地质大队，新疆哈密, 839000;吐哈油田勘探开发研究院，新疆哈密, 839009 |
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| 基金项目： | 国家自然科学基金项目（面上项目，重点项目，重大项目） |
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| 摘 要： | 对北山地区坡一和罗东含铜镍的镁铁-超镁铁质岩体铂族元素研究表明，两个岩体的铂族元素(PGE)总量较低，PPGE较IPGE富集，原始地幔标准化模式呈正斜率，均较原始地幔亏损，具Ir和Rh的弱负异常。较低的Pd/Ir比值表明岩石主要受岩浆作用控制，后期热液作用影响不明显。两个岩体的原生岩浆均为MgO 含量较高的PGE不亏损的拉斑玄武质岩浆，较高的Cu/Pd、Ti/Pd比值表明岩浆在演化过程中发生了硫化物的熔离。罗东岩体早期矿物相（橄榄石、铬铁矿）的分离结晶作用对岩浆中的硫达到饱和具有重要的贡献，而坡一岩体该作用对硫化物熔离的贡献不明显。坡一和罗东岩体的R值表明两岩体均具有达到中型Ni矿床的潜力。
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| 关 键 词： | 铂族元素 地球化学 成矿作用 镁铁-超镁铁质岩 新疆北山 |
| 收稿时间： | 2011/4/20 0:00:00 |
| 修稿时间： | 2011/7/23 0:00:00 |
Platinum Group Elements Geochemistry of Two Mafic Ultramafic Intrusions in the Beishan Block Xinjiang NW China |
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| CHAI Fengmei,XIA Fang,CHEN Bin,LU Hongfei,WANG Heng,LI Jun and YAN Yupu.Platinum Group Elements Geochemistry of Two Mafic Ultramafic Intrusions in the Beishan Block Xinjiang NW China[J].Acta Geologica Sinica,2013,87(4):474-485. |
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| Authors: | CHAI Fengmei XIA Fang CHEN Bin LU Hongfei WANG Heng LI Jun and YAN Yupu |
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| Institution: | Xinjiang University |
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| Abstract: | The contents of platinum group elements, Ni, Cu and MgO of Poyi and Luodong Ni-Cu sulphide-bearing mafic-ultramafic intrusions in the Beishan have been analyzed. The total PGE contents are quite low, ranging from 2.15×10-9 to 18.66×10-9 in Poyi intrusion and 0.55×10-9 to 3.18×10-9 in Luodong intrusion, respectively. The PGE primitive mantle-normalized patterns display a positive slop and low fractionation between IPGE and PPGE with negative Ir and Rh anomalies. The PGE, Cu and Ni are depleted relative to the primitive mantle with low and narrow Pd/Ir ranges (3.47-7.35 and 9.73-20.67) showing affected by magmatizm. The relationship between Ni/Cu and Pd/Ir indicated that the primary magma was high-magnesium tholeiitic. The Cu/Pd and Ti/Pd ratios of these rocks suggest that the primary magmas have underwent segragation of sulfide before their emplacement. The obviously positive correlation between Cr and Ni, Ir in Luodong intrusion showed that fractionation of olivine and chromite before segragation of sulfide, while the influence on PGE from crystallization differentiation in Poyi intrusion is unconspicuous. Based on the PGE model calculations, the calculated R values suggested that the two intrusions were potential to form middle Ni deposit. |
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| Keywords: | Platinum group element Geochemistry Ni-Cu mineralization mafic-ultramafic intrusions Beishan |
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