| 芬兰北部克维特斯塔镍-铜-铂族元素矿床地质特征及矿床成因 |
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| 引用本文： | 张晓康,聂凤军,徐九华,吴科锐.芬兰北部克维特斯塔镍-铜-铂族元素矿床地质特征及矿床成因[J].地质通报,2015,34(6):1146-1159. |
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| 作者姓名： | 张晓康 聂凤军 徐九华 吴科锐 |
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| 作者单位： | 1.北京科技大学土木与环境工程学院，北京 100083；2.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，北京 100037 |
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| 基金项目： | 中国地质调查局项目（编号：12120115065901、12120115068701、1212011120326） |
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| 摘 要： | 位于芬兰北部中拉普兰绿岩带的克维特斯塔(Kevitsa)镍-铜-铂族元素矿床是世界上主要的岩浆镍-铜硫化物矿床之一。该矿床储量大,含丰富的镍-铜硫化物和铂族元素。对矿床产出环境、地质特征、矿床成因等进行了总结,结果表明:矿体主要赋存于克维特斯塔基性—超基性层状侵入体的超基性单元中。主要矿石类型为普通型和镍-铂族元素型2种,其中镍-铂族元素型矿石内橄榄石具极高的Ni含量。主要矿石矿物为磁黄铁矿、镍黄铁矿、黄铜矿、黄铁矿、针硫镍矿、红砷镍矿、砷镍矿、辉砷镍矿等,绝大部分铂族矿物包含在硅酸盐中和附着在硫化物颗粒边界。Re-Os、Sm-Nd、Sr及S同位素特征显示成矿岩浆为幔源,但受到地壳物质的混染作用。Pb同位素年代学结果表明克维特斯塔侵入体形成于古元古代。
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| 关 键 词： | 镍-铜-铂族元素矿床 层状侵入体 中拉普兰绿岩带 橄榄石 芬兰 |
Geological characteristics and genesis of the Kevitsa Ni-Cu-PGE deposit, northern Finland |
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| ZHANG Xiaokang,NIE Fengjun,XU Jiuhu,WU Kerui.Geological characteristics and genesis of the Kevitsa Ni-Cu-PGE deposit, northern Finland[J].Geologcal Bulletin OF China,2015,34(6):1146-1159. |
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| Authors: | ZHANG Xiaokang NIE Fengjun XU Jiuhu WU Kerui |
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| Institution: | 1. Civil and Environmental Engineering School, University of Science and Technology Beijing, Beijing 100083, China;2. MRL Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China |
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| Abstract: | Located in the Central Lapland greenstone belt of northern Finland, the Kevitsa Ni-Cu-PGE deposit is one of the major magmatic Ni-Cu sulfide deposits in the world. The deposit has abundant reserves and is rich in Ni-Cu sulfide and PGE. This paper summarizes the environment, geological characteristics, ore genesis and other aspects of the ore deposit. The orebodies are mainly hosted in ultramafic unit in the Kevitsa mafic-ultramafic layered intrusions; the main ore types are divided into two types, i.e., common type and Ni-PGE type; the olivines in Ni-PGE type have extremely high Ni content; the main ore minerals include pyrrhotite, pentlandite, chalcopyrite, pyrite, millerite, niccolite, chloanthite and gersdorffite, with most of the platinum group minerals contained in the silicate or attached to the boundary of sulfide particles; Re-Os, Sm-Nd, Sr and S isotopic characteristics indicate that mineralized magma was derived from the mantle, but the magma was contaminated by crustal substances; geochronologic analysis indicates that Kevitsa intrusion was formed in the Paleoproterozoic. |
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| Keywords: | Ni-Cu-PGE deposit layered intrusions central Lapland greenstone belt olivine Finland |
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