内蒙古固阳绿岩带条带状铁建造地球化学特征与沉积环境讨论
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摘要
Algoma型条带状铁建造(BIF)是一种海相化学沉积岩,它发育在太古宙绿岩带的火山-沉积岩序列中,大部分经历了后期变质变形作用。稀土元素具有稳定的地球化学性质,因而被广泛用于指示BIF的原始沉积环境。华北克拉通北缘固阳绿岩带中的BIF(如三合明、公益明、东五分子、公巨成等)赋存于新太古代色尔腾山群的变火山-沉积序列中,普遍经历了绿片岩相—低角闪岩相变质,呈条带状构造,其主要矿物组成为自形—半自形粒状磁铁矿和他形粒状石英,含少量角闪石,局部地区可见石榴石、绿泥石、斜长石等富Al矿物。根据BIF中惰性元素的含量及其相关性,可划分为纯净的BIF和遭受碎屑物质混染的BIF,并通过特征的Co/Th比值判断出这些碎屑物质主要来自于玄武质岩石。纯净及遭受轻微碎屑物质混染的BIF稀土元素特征通过后太古宙页岩(PAAS)标准化后,与现代海水及其他地区典型太古宙BIF相似,均表现为轻稀土相对重稀土亏损,正La、Y异常以及较高的Y/Ho比值(>29)。大多数样品发育不明显的负Ce_(PAAS)异常,说明BIF沉淀自缺氧的环境;正Eu_(PAAS)异常明显,说明海水中有高温(>250℃)热液的加入,其比例为0~10%。然而,遭受强烈碎屑物质混染的BIF稀土元素特征则具有明显差异。此种类型BIF的出现及分布不均,指示了在BIF沉积之前的局部地区或时间段内,深部海水处于相对动荡的环境。
Algoma-type Banded Iron Formations(BIFs) are marine chemical sedimentary rocks that are generally interlayered with volcanic rocks and/or sedimentary sequences in Archean greenstone belts, mostly followed by metamorphism and deformation.Because rare earth elements(REEs) are usually not fractionated during diagenesis and metamorphism, REE patterns are thus regarded as a powerful tool to understand conditions under which BIF were deposited. Located in the northern North China Craton(NCC), BIFs such as Sanheming, Gongyiming, Dongwufenzi and Gongjucheng are hosted by the Guyang greenstone belt, of Seertengshan Group which consists of multiple sequences of metavolcanic rocks and metasedimentary rocks. The regional metamorphic grade ranges from upper greenschist-to lower amphibolite-facies. The BIFs are composed of laminated magnetite and white to gray quartz associated with amphibole layers. Moreover, minor chlorite, garnet and plagioclase, rich in Al, are observed interbedded with quartz and magnetite. Based on the content of immobile elements, the samples can be subdivided into two types:pure and contaminated. Cr/Th ratios in the contaminated BIF indicate that detritus is mainly from basaltic rocks. Normalized by post-Archean Australian Shale(PAAS), REE patterns of pure and weakly contaminated BIF are characterized by depletion of LREE,positive La and Y anomalies, and relatively high Y/Ho ratios(>29), which are typical of modern seawater and some other Archean BIF. Slightly negative CePAASanomalies are present in most samples, suggesting its precipitation from anoxic waters. Large positive EuPAASanomalies may indicate that, during deposition of BIF, the oceans were greatly influenced by high-temperature(>250℃)hydrothermal fluxes which accounted for 0-10%. However, REE patterns of highly contaminated BIF are obviously distinct.Disordered destitution of this kind of BIF indicates that deep water in limited regions or time was not quiet before the deposition of BIF.
Algoma-type Banded Iron Formations(BIFs) are marine chemical sedimentary rocks that are generally interlayered with volcanic rocks and/or sedimentary sequences in Archean greenstone belts, mostly followed by metamorphism and deformation.Because rare earth elements(REEs) are usually not fractionated during diagenesis and metamorphism, REE patterns are thus regarded as a powerful tool to understand conditions under which BIF were deposited. Located in the northern North China Craton(NCC), BIFs such as Sanheming, Gongyiming, Dongwufenzi and Gongjucheng are hosted by the Guyang greenstone belt, of Seertengshan Group which consists of multiple sequences of metavolcanic rocks and metasedimentary rocks. The regional metamorphic grade ranges from upper greenschist-to lower amphibolite-facies. The BIFs are composed of laminated magnetite and white to gray quartz associated with amphibole layers. Moreover, minor chlorite, garnet and plagioclase, rich in Al, are observed interbedded with quartz and magnetite. Based on the content of immobile elements, the samples can be subdivided into two types:pure and contaminated. Cr/Th ratios in the contaminated BIF indicate that detritus is mainly from basaltic rocks. Normalized by post-Archean Australian Shale(PAAS), REE patterns of pure and weakly contaminated BIF are characterized by depletion of LREE,positive La and Y anomalies, and relatively high Y/Ho ratios(>29), which are typical of modern seawater and some other Archean BIF. Slightly negative CePAASanomalies are present in most samples, suggesting its precipitation from anoxic waters. Large positive EuPAASanomalies may indicate that, during deposition of BIF, the oceans were greatly influenced by high-temperature(>250℃)hydrothermal fluxes which accounted for 0-10%. However, REE patterns of highly contaminated BIF are obviously distinct.Disordered destitution of this kind of BIF indicates that deep water in limited regions or time was not quiet before the deposition of BIF.
引文
Alexander B W,Bau M,Andersson P,Dulski,P.2008.Continentallyderived solutes in shallow Archean seawater:Rare earth element and Nd isotope evidence in iron formation from the 2.9Ga Pongola Supergroup,South Africa[J].Geochimica Et Cosmochimica Acta,72(2):378-394.
Alibo D S,Nozaki Y.1999.Rare earth elements in seawater:Particle association,shale-normalization,and Ce oxidation[J].Geochimica et Cosmochimica Acta,63(3/4):363-372.
Bau M,Dulski P.1996.Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations,Transvaal Supergroup,South Africa[J].Precambrian Research,79(/2):37-55.
Bau M,M?ller P.1993.Rare earth element systematics of the chemically precipitated component in early precambrian iron formations and the evolution of the terrestrial atmospherehydrosphere-lithosphere system[J].Geochimica et Cosmochimica Acta,57(10):2239-2249.
Bau M.1991.Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium[J].Chemical Geology,93(3/4):219-230.
Bekker A,Krapez B,Slack J,Planavsky N,Hofmann A,Konhauser KO,Rouxel O J.2010.Iron formation:The sedimentary product of a complex interplay among mantle,tectonic,oceanic,and biospheric processes-a reply[J].Economic Geology,105(3):467-508.
Bekker A,Planavsky N J,Krape?B,Konhauser K.2014.9.18-Iron Formations:Their origins and implications for ancient seawater chemistry[J].Treatise on Geochemistry,561-628.
Bolhar R,Kamber B S,Moorbath S,Fedo C M,Whitehouse M J.2004.Characterisation of early Archaean chemical sediments by trace element signatures[J].Earth&Planetary Science Letters,222(1):43-60.
Byrne R H,Sholkovitz E R.1996.Chapter 158 Marine chemistry and geochemistry of the lanthanides[J].Handbook on the Physics&Chemistry of Rare Earths,23:497-593.
Chen Zhiyong,Zheng Fanshen,Wang Zhong,Li Siwa,Wang Fukuan.2007.The Seertengshan Rock Group in middle-west Inner Mongolia:Revision and its geological significance[J].Geology and Resources,16(1):1-6(in Chinese).
Chen Liang.2007.Geochemistry and Chronology of the Guyang Greenstone Belt.Postdoctorial Research Report[D].Beijing:Institute of Geology and Geophysics,Chinese Academyof Sciences,1-40(in Chinese).
Condie K C,Wronkiewicz D J.1990.The Cr/Th ratio in Precambrian pelites from the Kaapvaal Craton as an index of craton evolution[J].Earth and Planetary Science Letters,97(3/4):256-267.
Dai Yanpei,Zhang Lianchang,Zhu Mingtian,Wang Changle,Liu Li.2013.Chentaigou BIF-type iron deposit,Anshan area associated with Archean crustal growth:Constraints from zircon U-Pb dating and Hf isotope[J].Acta Petrologica Sinica,29(7):2537-2550
Frei R,Polat A.2007.Source heterogeneity for the major components of~3.7 Ga Banded Iron Formations(Isua Greenstone Belt,Western Greenland):Tracing the nature of interacting water masses in BIFformation[J].Earth&Planetary Science Letters,253(1/2):266-281.
Fu Jianfei,Wang Ende,Xia Jianming,Men Yekai,Chen Huijun,You Xinwei,Chenglin.2014.Element geochemical characteristics and sedimentary palaeoenvironment of the Yanqianshan iron deposit in Liaoning Province[J].Geology in China,41(6):1929-1943(in Chinese with English abstract).
German C R,Elderfield H.1989.Rare earth elements in Saanich Inlet,British Columbia,a seasonally anoxic basin[J].Geochimica et Cosmochimica Acta,53(89):2561-2571.
Gourcerol B,Thurston P C,Kontak D J,C?té-Mantha O,Biczok J.2016.Depositional setting of Algoma-type banded iron formation[J].Precambrian Research,47-79.
Gross G A.1980.A classification of iron formations based on depositional environments[J].Canadian Mineralogist,18(1):215-222.
Haugaard R,Frei R,Stendal H,et al.2013.Petrology and geochemistry of the~2.9 Ga Itilliarsuk banded iron formation and associated supracrustal rocks,West Greenland:Source characteristics and depositional environment[J].Precambrian Research,229:150-176.
Hong Xiuwei,Pang Hongwei,Liu Xuewen.2010.Geological characteristics of the Dataigou iron deposit in Benxi,Liaoning Province[J].Geology in China,37(5):1426-1433(in Chinese with English abstract).
Huston D L,Logan G A.2004.Barite,BIFs and bugs:Evidence for the evolution of the Earth’s early hydrosphere[J].Earth&Planetary Science Letters,220(1/2):41-55.
Isley A E,Abbott D H.1999.Plume-related mafic volcanism and the deposition of banded iron formation[J].Journal of Geophysical Research Atmospheres,1041(B7):15461-15477.
Jian Ping,Zhang Qi,Liu Dunyi,Jin Weijun,Jia Xiuqin,Qian Qing.2005.SHRIMP dating and geological significance of Late Achaean high-Mg diorite(sanukite)and hornblende-granite at Guyang of Inner Mongolia[J].Acta Petrol.Sin.,21(1):151-157(in Chinese with English abstract).
Klein C.2005.Some Precambrian banded iron-formations(BIFs)from around the world:Their age,geologic setting,mineralogy,metamorphism,geochemistry,and origin[J].American Mineralogist,90(10):1473-1499.
Klinkhammer G,Elderfield H,Hudson A.Rare earth elements in seawater near hydrothermal vents[J].Nature,1983,305(5931):185-188.
Li H,Zhang Z,Li L,Zhang Z,Chen J,Yao T.2014.Types and general characteristics of the BIF-related iron deposits in China[J].Ore Geology Reviews,57(3):264-287.
Li Houmin,Wang Denghong,Li Lixing.2012.Metallogeny ofiron deposits and resource potential of major iron minerogenetic units in China[J].Geology in China,39(3):559-580(in Chinese with English abstract).
Li Shuxun,Liu Xishan,Zhang Lüqiao.1987.Granite-greenstone belt in Sheerteng area,Inner Mongolia,China[J].Changchun Univ.Geol.,(17):81-102(in Chinese with English abstract).
Liu Jianzhong,Zhang Fuqin,Ouyang Ziyuan,Li Chunlai,Zou Yongliao,Xu lin.2001.Study on Geochemistry and Choronology of Seertengshan Greenstone,Inner Mongolia[J].Journal of Changchun University of Science and Technology,31(3):236-240(in Chinese with English abstract).
Liu L,Zhang L,Dai Y.2014.Formation age and genesis of the banded iron formations from the Guyang Greenstone Belt,Western North China Craton[J].Ore Geology Reviews,63(1):388-404.
Liu Li.,Zhang Lianchang,Dai Yanpei,Wang Changle,Wang Changle,Li Zhiquan.2012.Formation age,geochemical signaturesand geological significance of the Sanheming BIF-type iron deposit in the Guyang Greenstone Belt,Inner Mongolia[J].Acta Petrol.Sin.,28(11):3623-3637(in Chinese with English abstract).
Liu Mingjun,Li Houmin,Yu Shixiang,Xu Zongxian,Yao Liangde,Wen Qi,Zhao Hongzhen.2014.Re-Os isotopic dating of pyrite and molybdenite from the iron deposits in Anshan-Benxi area of Liaoning Province and its geological significances[J].Geology in China,41(6):1821-1832(in Chinese with English abstract).
Liu Xishan.Progressive Metamorphic Genesis of Archean Granulites in Central Nei Monglo[J].Acta Petrol.Sin.,1996(2):287-298(in Chinese).
Ma X D,Fan H R,Santosh M,Guo J.2014.Chronology and geochemistry of Neoarchean BIF-type iron deposits in the Yinshan Block,North China Craton:Implications for oceanic ridge subduction[J].Ore Geology Reviews,63(1):405-417.
Ma Xudong,Fan Hongrui,Guo Jinghui.2013.Neoarchean magmatism,metamorphism in the Yinshan Block:Implication for the genesis of BIF and crustal evolution[J].Acta Petrol.Sina,29(7):2329-2339(in Chinese with English abstract).
Meng Xuyang,Wang Peng,Zhang Dongyang,Liang Mingjuan.2012.Element geochemistry of the Sishanling iron deposit in Liaoning Province and its geological implications[J].Geology in China,39(6):1857-1873(in Chinese with English abstract).
Nutman A P,Fryer B J,Bridgwater D.2011.The early Archaean Nulliak(supracrustal)assemblage,northern Labrador[J].Canadian Journal of Earth Sciences,26(10):2159-2168.
Nutman A P.1986.The early Archaean to Proterozoic history of the Isukasia area,southern West Greenland[J].
Planavsky N,Bekker A,Rouxel O J,Kamber B,Hofmann A,Knudsen A,Lyons T W.2010.Rare Earth Element and yttrium compositions of Archean and Paleoproterozoic Fe formations revisited:New perspectives on the significance and mechanisms of deposition[J].Geochimica et Cosmochimica Acta,74(22):6387-6405.
Taylor S R,Mclennan S M.1984.The Continental Crust:Its Composition and Evolution[J].Journal of Geology,94(4).
Thurston P C,Kamber B S,Whitehouse M.2012.Archean cherts in banded iron formation:Insight into Neoarchean ocean chemistry and depositional processes[J].Precambrian Research,214-215(3):227-257.
Viehmann S,Bau M,Smith A J B,Beukes N J,Dantas E L,Bühn B.2015.The reliability of~2.9 Ga old Witwatersrand banded iron formations(South Africa)as archives for Mesoarchean seawater:Evidence from REE and Nd isotope systematics[J].Journal of African Earth Sciences,111(5):322-334.
Wang C,Konhauser K O,Zhang L.2015.Depositional environment of the Paleoproterozoic Yuanjiacun banded iron formation in Shanxi Province,China[J].Economic Geology,110(6):1515-1539.
Wang Changle,Zhang Lianchang,Lan Caiyun,Dai Yanpei.2014.Rare earth element and yttrium compositions of the Paleoproterozoic Yuanjiacun BIF in the Lüliang area and their implications for the Great Oxidation Event(GOE)[J].Science China:Earth Sciences,57:2469-2485.
Yao Peihui.1993.Iron Deposits of China[M].Beijing:Metallurgical Industry Press,219-241(in Chinese).
Zhai Mingguo,Bian Aiguo.2000.The supercontinent amalgamation of the North China cratonin the Late Archean and breaking up in the Paleoproterozoic to Mesoproterozoic[J].Sci.China,30(B12):129-137.(in Chinese).
Zhang Lianchang,Zhai Mingguo,Wan Yusheng,Guo Jinghui,Dai Yanpei,Wang Changle,Liu Li.2012.Study of the Precambrian BIF-iron deposits in the North China Craton:Progresses and questions[J].Acta Petrol.Sin.,28(11):3431-3445(in Chinese with English abstract).
陈亮.2007.固阳绿岩带的地球化学和年代学[D].北京:中国科学院地质与地球物理研究所,1-40.
陈志勇,郑翻身,王忠,李四娃,王富宽.2007.内蒙古中西部色尔腾山岩群的厘定及其地质意义[J].地质与资源,16(1):1-6.
代堰锫,张连昌,朱明田,王长乐,刘利.2013.鞍山陈台沟BIF铁矿与太古代地壳增生:锆石U-Pb年龄与Hf同位素约束[J].岩石学报,29(07):2537-2550.
付建飞,王恩德,夏建明,门业凯,陈慧钧,尤欣慰,成林.2014.辽宁眼前山铁矿元素地球化学特征与沉积古环境研究[J].中国地质,41(6):1929-1943.
洪秀伟,庞宏伟,刘学文.2010.辽宁本溪大台沟铁矿地质特征[J].中国地质,37(5):1426-1433.
简平,张旗,刘敦一,金维浚,贾秀勤,钱青.2005.内蒙古固阳晚太古代赞岐岩(sanukite)--角闪花岗岩的SHRIMP定年及其意义[J].岩石学报,21(01):151-157.
李厚民,王登红,李立兴,陈靖,杨秀清,刘明军.2012.中国铁矿成矿规律及重点矿集区资源潜力分析[J].中国地质,39(3):559-580.
李树勋,刘喜山,张履桥.1987.内蒙古色尔腾山地区花岗岩-绿岩的地质特征[J].长春地质学院学报,81-102.
刘建忠,张福勤,欧阳自远,李春来,邹永廖,徐琳.2001.内蒙古色尔腾山绿岩的地球化学、年代学研究[J].长春科技大学学报,31(3):236-240.
刘利,张连昌,代堰锫,王长乐,李智泉.2012.内蒙古固阳绿岩带三合明BIF型铁矿的形成时代、地球化学特征及地质意义[J].岩石学报,28(11):3623-3637.
刘明军,李厚民,于仕祥,许宗宪,姚良德,文屹,赵洪振.2014.辽宁鞍本地区铁矿床黄铁矿和辉钼矿Re-Os同位素测年及其地质意义[J].中国地质,41(6):1821-1832.
刘喜山.1996.内蒙古中部太古代麻粒岩递增变质成因[J].岩石学报,(2):287-298.
马旭东,范宏瑞,郭敬辉.2013.阴山地块晚太古代岩浆作用、变质作用对地壳演化及BIF成因的启示[J].岩石学报,29(7):2329-2339.
孟旭阳,王鹏,张东阳,梁明娟.2012,辽宁思山岭铁矿元素地球化学特征及其地质意义[J].中国地质,39(6):1857-1873.
王长乐,张连昌,兰彩云,代堰锫.2014.山西吕梁古元古代袁家村铁矿BIF稀土元素地球化学及其对大氧化事件的指示[J].中国科学:地球科学,44(11):2389-2405.
姚培慧.1993.中国铁矿志[M].北京:冶金工业出版社.
翟明国,卞爱国.2000.华北克拉通新太古代末超大陆拼合及古元古代末-中元古代裂解[J].中国科学,30(B12):129-137.
张连昌,翟明国,万渝生,郭敬辉,代堰锫,王长乐,刘利.2012.华北克拉通前寒武纪BIF铁矿研究:进展与问题[J].岩石学报,28(11):3431-3445.
Alibo D S,Nozaki Y.1999.Rare earth elements in seawater:Particle association,shale-normalization,and Ce oxidation[J].Geochimica et Cosmochimica Acta,63(3/4):363-372.
Bau M,Dulski P.1996.Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations,Transvaal Supergroup,South Africa[J].Precambrian Research,79(/2):37-55.
Bau M,M?ller P.1993.Rare earth element systematics of the chemically precipitated component in early precambrian iron formations and the evolution of the terrestrial atmospherehydrosphere-lithosphere system[J].Geochimica et Cosmochimica Acta,57(10):2239-2249.
Bau M.1991.Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium[J].Chemical Geology,93(3/4):219-230.
Bekker A,Krapez B,Slack J,Planavsky N,Hofmann A,Konhauser KO,Rouxel O J.2010.Iron formation:The sedimentary product of a complex interplay among mantle,tectonic,oceanic,and biospheric processes-a reply[J].Economic Geology,105(3):467-508.
Bekker A,Planavsky N J,Krape?B,Konhauser K.2014.9.18-Iron Formations:Their origins and implications for ancient seawater chemistry[J].Treatise on Geochemistry,561-628.
Bolhar R,Kamber B S,Moorbath S,Fedo C M,Whitehouse M J.2004.Characterisation of early Archaean chemical sediments by trace element signatures[J].Earth&Planetary Science Letters,222(1):43-60.
Byrne R H,Sholkovitz E R.1996.Chapter 158 Marine chemistry and geochemistry of the lanthanides[J].Handbook on the Physics&Chemistry of Rare Earths,23:497-593.
Chen Zhiyong,Zheng Fanshen,Wang Zhong,Li Siwa,Wang Fukuan.2007.The Seertengshan Rock Group in middle-west Inner Mongolia:Revision and its geological significance[J].Geology and Resources,16(1):1-6(in Chinese).
Chen Liang.2007.Geochemistry and Chronology of the Guyang Greenstone Belt.Postdoctorial Research Report[D].Beijing:Institute of Geology and Geophysics,Chinese Academyof Sciences,1-40(in Chinese).
Condie K C,Wronkiewicz D J.1990.The Cr/Th ratio in Precambrian pelites from the Kaapvaal Craton as an index of craton evolution[J].Earth and Planetary Science Letters,97(3/4):256-267.
Dai Yanpei,Zhang Lianchang,Zhu Mingtian,Wang Changle,Liu Li.2013.Chentaigou BIF-type iron deposit,Anshan area associated with Archean crustal growth:Constraints from zircon U-Pb dating and Hf isotope[J].Acta Petrologica Sinica,29(7):2537-2550
Frei R,Polat A.2007.Source heterogeneity for the major components of~3.7 Ga Banded Iron Formations(Isua Greenstone Belt,Western Greenland):Tracing the nature of interacting water masses in BIFformation[J].Earth&Planetary Science Letters,253(1/2):266-281.
Fu Jianfei,Wang Ende,Xia Jianming,Men Yekai,Chen Huijun,You Xinwei,Chenglin.2014.Element geochemical characteristics and sedimentary palaeoenvironment of the Yanqianshan iron deposit in Liaoning Province[J].Geology in China,41(6):1929-1943(in Chinese with English abstract).
German C R,Elderfield H.1989.Rare earth elements in Saanich Inlet,British Columbia,a seasonally anoxic basin[J].Geochimica et Cosmochimica Acta,53(89):2561-2571.
Gourcerol B,Thurston P C,Kontak D J,C?té-Mantha O,Biczok J.2016.Depositional setting of Algoma-type banded iron formation[J].Precambrian Research,47-79.
Gross G A.1980.A classification of iron formations based on depositional environments[J].Canadian Mineralogist,18(1):215-222.
Haugaard R,Frei R,Stendal H,et al.2013.Petrology and geochemistry of the~2.9 Ga Itilliarsuk banded iron formation and associated supracrustal rocks,West Greenland:Source characteristics and depositional environment[J].Precambrian Research,229:150-176.
Hong Xiuwei,Pang Hongwei,Liu Xuewen.2010.Geological characteristics of the Dataigou iron deposit in Benxi,Liaoning Province[J].Geology in China,37(5):1426-1433(in Chinese with English abstract).
Huston D L,Logan G A.2004.Barite,BIFs and bugs:Evidence for the evolution of the Earth’s early hydrosphere[J].Earth&Planetary Science Letters,220(1/2):41-55.
Isley A E,Abbott D H.1999.Plume-related mafic volcanism and the deposition of banded iron formation[J].Journal of Geophysical Research Atmospheres,1041(B7):15461-15477.
Jian Ping,Zhang Qi,Liu Dunyi,Jin Weijun,Jia Xiuqin,Qian Qing.2005.SHRIMP dating and geological significance of Late Achaean high-Mg diorite(sanukite)and hornblende-granite at Guyang of Inner Mongolia[J].Acta Petrol.Sin.,21(1):151-157(in Chinese with English abstract).
Klein C.2005.Some Precambrian banded iron-formations(BIFs)from around the world:Their age,geologic setting,mineralogy,metamorphism,geochemistry,and origin[J].American Mineralogist,90(10):1473-1499.
Klinkhammer G,Elderfield H,Hudson A.Rare earth elements in seawater near hydrothermal vents[J].Nature,1983,305(5931):185-188.
Li H,Zhang Z,Li L,Zhang Z,Chen J,Yao T.2014.Types and general characteristics of the BIF-related iron deposits in China[J].Ore Geology Reviews,57(3):264-287.
Li Houmin,Wang Denghong,Li Lixing.2012.Metallogeny ofiron deposits and resource potential of major iron minerogenetic units in China[J].Geology in China,39(3):559-580(in Chinese with English abstract).
Li Shuxun,Liu Xishan,Zhang Lüqiao.1987.Granite-greenstone belt in Sheerteng area,Inner Mongolia,China[J].Changchun Univ.Geol.,(17):81-102(in Chinese with English abstract).
Liu Jianzhong,Zhang Fuqin,Ouyang Ziyuan,Li Chunlai,Zou Yongliao,Xu lin.2001.Study on Geochemistry and Choronology of Seertengshan Greenstone,Inner Mongolia[J].Journal of Changchun University of Science and Technology,31(3):236-240(in Chinese with English abstract).
Liu L,Zhang L,Dai Y.2014.Formation age and genesis of the banded iron formations from the Guyang Greenstone Belt,Western North China Craton[J].Ore Geology Reviews,63(1):388-404.
Liu Li.,Zhang Lianchang,Dai Yanpei,Wang Changle,Wang Changle,Li Zhiquan.2012.Formation age,geochemical signaturesand geological significance of the Sanheming BIF-type iron deposit in the Guyang Greenstone Belt,Inner Mongolia[J].Acta Petrol.Sin.,28(11):3623-3637(in Chinese with English abstract).
Liu Mingjun,Li Houmin,Yu Shixiang,Xu Zongxian,Yao Liangde,Wen Qi,Zhao Hongzhen.2014.Re-Os isotopic dating of pyrite and molybdenite from the iron deposits in Anshan-Benxi area of Liaoning Province and its geological significances[J].Geology in China,41(6):1821-1832(in Chinese with English abstract).
Liu Xishan.Progressive Metamorphic Genesis of Archean Granulites in Central Nei Monglo[J].Acta Petrol.Sin.,1996(2):287-298(in Chinese).
Ma X D,Fan H R,Santosh M,Guo J.2014.Chronology and geochemistry of Neoarchean BIF-type iron deposits in the Yinshan Block,North China Craton:Implications for oceanic ridge subduction[J].Ore Geology Reviews,63(1):405-417.
Ma Xudong,Fan Hongrui,Guo Jinghui.2013.Neoarchean magmatism,metamorphism in the Yinshan Block:Implication for the genesis of BIF and crustal evolution[J].Acta Petrol.Sina,29(7):2329-2339(in Chinese with English abstract).
Meng Xuyang,Wang Peng,Zhang Dongyang,Liang Mingjuan.2012.Element geochemistry of the Sishanling iron deposit in Liaoning Province and its geological implications[J].Geology in China,39(6):1857-1873(in Chinese with English abstract).
Nutman A P,Fryer B J,Bridgwater D.2011.The early Archaean Nulliak(supracrustal)assemblage,northern Labrador[J].Canadian Journal of Earth Sciences,26(10):2159-2168.
Nutman A P.1986.The early Archaean to Proterozoic history of the Isukasia area,southern West Greenland[J].
Planavsky N,Bekker A,Rouxel O J,Kamber B,Hofmann A,Knudsen A,Lyons T W.2010.Rare Earth Element and yttrium compositions of Archean and Paleoproterozoic Fe formations revisited:New perspectives on the significance and mechanisms of deposition[J].Geochimica et Cosmochimica Acta,74(22):6387-6405.
Taylor S R,Mclennan S M.1984.The Continental Crust:Its Composition and Evolution[J].Journal of Geology,94(4).
Thurston P C,Kamber B S,Whitehouse M.2012.Archean cherts in banded iron formation:Insight into Neoarchean ocean chemistry and depositional processes[J].Precambrian Research,214-215(3):227-257.
Viehmann S,Bau M,Smith A J B,Beukes N J,Dantas E L,Bühn B.2015.The reliability of~2.9 Ga old Witwatersrand banded iron formations(South Africa)as archives for Mesoarchean seawater:Evidence from REE and Nd isotope systematics[J].Journal of African Earth Sciences,111(5):322-334.
Wang C,Konhauser K O,Zhang L.2015.Depositional environment of the Paleoproterozoic Yuanjiacun banded iron formation in Shanxi Province,China[J].Economic Geology,110(6):1515-1539.
Wang Changle,Zhang Lianchang,Lan Caiyun,Dai Yanpei.2014.Rare earth element and yttrium compositions of the Paleoproterozoic Yuanjiacun BIF in the Lüliang area and their implications for the Great Oxidation Event(GOE)[J].Science China:Earth Sciences,57:2469-2485.
Yao Peihui.1993.Iron Deposits of China[M].Beijing:Metallurgical Industry Press,219-241(in Chinese).
Zhai Mingguo,Bian Aiguo.2000.The supercontinent amalgamation of the North China cratonin the Late Archean and breaking up in the Paleoproterozoic to Mesoproterozoic[J].Sci.China,30(B12):129-137.(in Chinese).
Zhang Lianchang,Zhai Mingguo,Wan Yusheng,Guo Jinghui,Dai Yanpei,Wang Changle,Liu Li.2012.Study of the Precambrian BIF-iron deposits in the North China Craton:Progresses and questions[J].Acta Petrol.Sin.,28(11):3431-3445(in Chinese with English abstract).
陈亮.2007.固阳绿岩带的地球化学和年代学[D].北京:中国科学院地质与地球物理研究所,1-40.
陈志勇,郑翻身,王忠,李四娃,王富宽.2007.内蒙古中西部色尔腾山岩群的厘定及其地质意义[J].地质与资源,16(1):1-6.
代堰锫,张连昌,朱明田,王长乐,刘利.2013.鞍山陈台沟BIF铁矿与太古代地壳增生:锆石U-Pb年龄与Hf同位素约束[J].岩石学报,29(07):2537-2550.
付建飞,王恩德,夏建明,门业凯,陈慧钧,尤欣慰,成林.2014.辽宁眼前山铁矿元素地球化学特征与沉积古环境研究[J].中国地质,41(6):1929-1943.
洪秀伟,庞宏伟,刘学文.2010.辽宁本溪大台沟铁矿地质特征[J].中国地质,37(5):1426-1433.
简平,张旗,刘敦一,金维浚,贾秀勤,钱青.2005.内蒙古固阳晚太古代赞岐岩(sanukite)--角闪花岗岩的SHRIMP定年及其意义[J].岩石学报,21(01):151-157.
李厚民,王登红,李立兴,陈靖,杨秀清,刘明军.2012.中国铁矿成矿规律及重点矿集区资源潜力分析[J].中国地质,39(3):559-580.
李树勋,刘喜山,张履桥.1987.内蒙古色尔腾山地区花岗岩-绿岩的地质特征[J].长春地质学院学报,81-102.
刘建忠,张福勤,欧阳自远,李春来,邹永廖,徐琳.2001.内蒙古色尔腾山绿岩的地球化学、年代学研究[J].长春科技大学学报,31(3):236-240.
刘利,张连昌,代堰锫,王长乐,李智泉.2012.内蒙古固阳绿岩带三合明BIF型铁矿的形成时代、地球化学特征及地质意义[J].岩石学报,28(11):3623-3637.
刘明军,李厚民,于仕祥,许宗宪,姚良德,文屹,赵洪振.2014.辽宁鞍本地区铁矿床黄铁矿和辉钼矿Re-Os同位素测年及其地质意义[J].中国地质,41(6):1821-1832.
刘喜山.1996.内蒙古中部太古代麻粒岩递增变质成因[J].岩石学报,(2):287-298.
马旭东,范宏瑞,郭敬辉.2013.阴山地块晚太古代岩浆作用、变质作用对地壳演化及BIF成因的启示[J].岩石学报,29(7):2329-2339.
孟旭阳,王鹏,张东阳,梁明娟.2012,辽宁思山岭铁矿元素地球化学特征及其地质意义[J].中国地质,39(6):1857-1873.
王长乐,张连昌,兰彩云,代堰锫.2014.山西吕梁古元古代袁家村铁矿BIF稀土元素地球化学及其对大氧化事件的指示[J].中国科学:地球科学,44(11):2389-2405.
姚培慧.1993.中国铁矿志[M].北京:冶金工业出版社.
翟明国,卞爱国.2000.华北克拉通新太古代末超大陆拼合及古元古代末-中元古代裂解[J].中国科学,30(B12):129-137.
张连昌,翟明国,万渝生,郭敬辉,代堰锫,王长乐,刘利.2012.华北克拉通前寒武纪BIF铁矿研究:进展与问题[J].岩石学报,28(11):3431-3445.