王丰翔;聂凤军;张伟波;曹毅;解小颖;

• 1:石家庄经济学院研究生学院
• 2:中国地质科学院矿产资源研究所
• 3:中国地质大学地球科学与资源学院

摘要(Abstract)：

基律纳铁矿床位于瑞典北部拉普兰地区,是迄今为止世界上产于中-基性火山岩中规模最大的磷灰石-磁铁矿建造矿床,也是欧洲目前唯一正在开采的特大型铁矿山。研究表明,基律纳铁矿床受构造-岩浆控制作用明显,多产在古元古代花岗质绿片岩体内。矿体与围岩呈整合接触,在两者的接触带上,普遍发育钠长石化和钾长石化;矿石以高度富集磁铁矿和磷灰石为特征。根据切割关系和锆石U-Pb同位素测年,其成矿年龄为1.9~1.88Ga。依据其地质背景、围岩蚀变分带性和成矿流体的组分特征,将该矿床初步认定为铁氧化物IOCG型铁矿床。

关键词(KeyWords)： 铁矿;基律纳;IOCG型矿床;地质特征;磷灰石-磁铁矿建造

Abstract:

Keywords:

基金项目(Foundation): 中国地质调查局项目“全球巨型成矿带区域构造与成矿地质背景对比研究”(1212011120326)

作者(Author): 王丰翔;聂凤军;张伟波;曹毅;解小颖;

Email:

DOI:

参考文献(References)：

• [1]河北钢铁集团矿业有限公司.瑞典LKAB公司基律纳铁矿考察报告[R].石家庄:河北钢铁集团矿业有限公司,2010.
• [2]谢理,焦玉书.今日瑞典基律纳铁矿[J].中国矿业,2003,12(4):46-47.
• [3]聂凤军,石成龙,赵元艺,等.北极圈及邻区金属矿床地质特征、形成作用与找矿潜力[J].中国地质,2012,39(4):856-868.
• [4]Weihed P,Eilu P,Larsen R B,et al.Metallic mineral deposits in the Nordic countries[J].Episodes,2008,31(1):125-132.
• [5]Weihed P,Arndt N,BillstrK,et al.Precambrian geodynamicsand ore formation:The Fennoscandian Shield[J].Ore Geology Reviews,2005,27:273-322.
• [6]Hitzman M W,Oreskes.N,Einaudi M.Geological characteristics and tectonic setting of Proterozoic iron oxide(Cu-U-AuREE)deposits[J].Precambrian Research,1992,58:241-287.
• [7]汪建.瑞典基律纳铁矿考察报告[J].矿业工程,2011,9(1):57-58.
• [8]弗里奇R.芬兰、挪威和瑞典矿床综述[J].盛乃贤,译.地质地球化学,1978,73(4):17-28.
• [9]Martinsson O.Paleoproterozoic greenstones at Kiruna in northern Sweden:A product of continental rifting and associated mafic-ultramafic volcanism:Paper I.Tectonic setting and metallogeny of the Kiruna greenstones[D].[S.l.]:Lulea University of Technology,1997.
• [10]Witschard F.The geological and tectonic evolution of the Precambrian of northern Sweden:A case for basement reactivation[J].Precambrian Research,1984,23:273-315.
• [11]Juhlin C,Elming S A,Mellqvist C,et al.Crustal reflectivity near the Archaean-Proterozoic boundary in northern Sweden and implications for the tectonic evolution of the area[J].Geophysical Journal International,2002,150:180-197.
• [12]Bergman S,Kubler L,Martinsson O.Description of regional geological and geophysical maps of northern Norrbotten County(east of the Caledonian orogen)[J].Sveriges Geologiske Undersokning,Ba,2001,56:110
• [13]Parák T.The origin of the Kiruna Iron Ores[J].Sveriges Geologiska Underskning,1975,C709:209.
• [14]Vollmer F W,Wright S F,Hudleston P J.Early deformation in the Svecokarelian greenstone belt of the Kiruna iron district,northern Sweden[J].Geologiska Freningens Istockholm Frhandlingar,1984,106(2):109-118.
• [15]Mai-Britt J,Sten-ke E.A correlation of AMS and rock quality in crystalline and sedimentary rocks in the Kirunavaara hanging wall,Sweden[J].Journal of Applied Geophysics,2012,86:54-69.
• [16]Edfelt,Armstrong R N,Smith M,et al.Alteration paragenesis and mineral chemistry of the Tjrrojkka apatite-iron and Cu(-Au)occurrences,Kiruna area,northern Sweden[J].Mineralium Deposita,2005,40:409-434.
• [17]Harlov D E,Andersson U B,Oerster F,et al.Apatite-monazite relations in the Kirunavaara magnetite-apatite ore,northern Sweden[J].Chemical Geology,2002,191:47-72.
• [18]Geijer P,dman O H.The emplacement of the Kiruna iron ores and related deposits[J].Sveriges Geologiska Underskning,1974,C700:48.
• [19]Rudyard F,Perdahl,Anders J.Rare earth elements in apatite and magnetite in Kiruna-type iron ores and some other iron ore types[J].Ore Geology Reviews,1995,9(6):489-510.
• [20]Cliff R A,David R,Blake K.Isotope systematics of the Kiruna magnetite ores,Sweden:Part 1.Age of the ore[J].Economic Geology,1990,85:1770-1776.
• [21]Sillitoe R H.Iron oxide-copper-gold deposits:An Andean view[J].Mineralium Deposita,2003,38:787-812.
• [22]余金杰,毛景文.Kiruna型铁矿床基本地质特征和成矿环境[J].矿床地质,2001,21(增):83-86.
• [23]毛景文,张作衡,王义天.国外主要矿床类型、特点及找矿勘查[M].北京:地质出版社,2012:126-137.
• [24]宋学信,陈毓川,盛继福,等.论火山浅成矿浆铁矿床[J].地质学报,1981,1:42-52.
• [25]聂凤军,江思宏,路彦明.氧化铁型铜-金(IOCG)矿床的地质特征、成因机理与找矿模型[J].中国地质,2008,26(8):1076-1087.
• [26]Alessandro S,Sten-ke E.Geophysical and petrophy sical study of an iron oxide copper gold deposit in northern Sweden[J].Ore Geology Reviews,2006,29:1-18.