第4期丁文君等:河北遷安杏山鐵礦床地球化學特征及其對成礦物質來源的指示365圖1遷安地區(qū)地質簡圖及其大地構造位置圖Fig.1SimplifiedgeologicalmapofQian’anareaanditsgeologicalsetting1.第四系;2.古近系新集組;3.上侏羅統(tǒng);4.中元古界;5.中太古界三屯營組;6.磁鐵石英巖;7.斷層第４期［２３］丁文君等：河北遷安杏山鐵礦床地球化學特征及其對成礦物質來源的指示３７３ｃｒｕｓｔＤａｎｉｅｌｓｏｎＡ，ＭｉｌｅｒＰ，ＤｕｌｓｋｉＰ．Ｔｈｅｅｕｒｏｐｉｕｍａｎｏｍａｌｉｅｓｉｎｂａｎｄｅｄｉｒｏｎｆｏｒｍａｔｉｏｎｓａｎｄｔｈｅｔｈｅｒｍａｌｈｉｓｔｏｒｙｏｆｔｈｅｏｃｅａｎｉｃ［Ｊ］．ＣｈｅｍｉｃａｌＧｅｏｌｏｇｙ，１９９２，９７：８９—１００．［２４］ＮｏｚａｋｉＹ，ＺｈａｎｇＪ，ＡｍａｋａｗａＨ．Ｔ｝ｌｅｆｒａｃｔｉｏｎａｔｉｏｎｂｅｔｗｅｅｎＹａｎｄＨｏｉｎｔｈｅｍａｒｉｎｅｅｎｖｉｒｏｎｍｅｎｔ［Ｊ］．ＥａｒｔｈａｎｄＰｌａｎｅｔａｒｙＳｃｉｅｎｃｅＬｅｔｔｅｒｓ，１９９７，１４８：３２９—３４０．［２５］李志紅，朱祥坤，唐索寒．鞍山——本溪地區(qū)條帶狀鐵建造的鐵同位素與稀土元素特征及其對成礦物質來源的指示［Ｊ］．巖石礦物學雜志，２００８，７（４）：２８５～２９０．ＬＩＺｈｉ－ｈｏｎｇ，ＺＨＵＸｉａｎｇ－ｋｕｎ，ＴＡＮＧＳｕｏ?ｈａｎ．ＣｈａｒａｃｔｅｒｓｏｆＦｅｉｓｏｔｏｐｅｓｅｔａｎｄｒａｒｅｅａｒｔｈｅｌｅｍｅｎｔｓｏｆｂａｎｄｅｄｉｒｏｎｆｏｒｍａｔｉｏｎｓｆｒｏｍＡｎｓｈａｎ－Ｂｅｎｘｉａｒｅａ：ｉｍｐｌｉｃａｔｉｏｎｓｆｏｒＦｅｓｏｕｒｃｅ［Ｊ］．ＡｃｔａＰｅｔｒｏｌｏｇｉｃａＭｉｎｅｒａｌｏｇｉｃａ，２００８，７（４）：２８５—２９０．［２６］ＦｒａｎｃｏＰ，ＬｅｏｎＢ．ＡｒｅｖｉｅｗｏｆＡｕｓｔｒａｌｉａ’ｓＰｒｏｔｅｒｏｚｏｉｃｍｉｎｅｒａｌｓｙｓｔｅｍｓａｎｄｇｅｎｅｔｉｃｍｏｄｅｌｓ［Ｊ］．ＰｒｅｃａｍｂｒｉａｎＲｅｓｅａｒｃｈ，２００８，１６６：５４—８０．［２７］趙斌，李統(tǒng)錦．鞍山弓長嶺富磁鐵礦床的形成機制和物理化學條件研究［Ｊ］．地球化學，１９８０，４：３３３。３“．ＺｈａｏＢｉｎ，ＬｉｉｒｏｎＴｏｎｇ－ｊｉｎ．ＡｐｒｅｌｉｍｉｎａｒｙｓｔｕｄｙｏｎｔｈｅｍｅｃｈａｎｉｓｍａｎｄｐｈｙｓｉｃｏｃｈｅｍｉｃａｌｃｏｎｄｉｔｉｏｎｓｏｆｆｏｒｍａｔｉｏｎｏｆＧｏｎｇｃｈａｎｇｌｉｎｇｒｉｃｈｄｅｐｏｓｉｔ［Ｊ］．Ｇｅｏｃｈｉｍｉｅａ，１９８０，４：３３３—３４４．［２８］鞠振南，衛(wèi)廣遠，劉鳳英．遼陽弓長嶺富鐵礦的成因探討［Ｊ］．黑龍江科技信息，２００９，１６：５３—５４．ｊｕＺｈｅｎ－ｎａｎ，ＷＥＩＧｕａｎｇ－ｙｕａｎ，ＬＩＵＦｅｎｇ－ｙｉｎｇ．ＴｈｅｓｔｕｄｙｏｎｔｈｅｃａｕｓｅｏｆｔｈｅＧｅｎｇｃｈａｎｇｌｉｎｇｈｉｇｈ－ｇｒａｄ＂ｉｒｏｎｄｅｐｏｓｉｔｏｆＬｉａｏｙａｎｇ［Ｊ］．Ｈｅｉｌｏｎｇｊｉａｎｇ［２９］ＳｃｉｅｎｃｅａｎｄＴｅｃｈｎｏｌｏｇｙＩｎｆｏｒｍａｔｉｏｎ，２００９，１６：５３—５４．關廣岳．風化淋濾型富鐵礦床的地球化學［Ｊ］．地質與勘探，１９７６，８：４—２４．ＧＵＡＮＧｕａｎｇ－）ｒｕｅ．ＧｅｏｃｈｅｍｉｓｔｒｙｏｆｗｅａｔｈｅｒｅｄｔｙｐｅｏｆＨｉｓｈ－Ｇｒａｄｅｏｒｅｄｅｐｏｓｉｔ［Ｊ］．ＧｅｏｌｏｇｙａｎｄＰｒｏｓｐｅｃｔｉｎｇ，１９７６，８：４—２４．ＧＥｏＣＨＥＭＩＣＡＬＣＨＡＲＡＣＴＥＲＳＦＲＯＭＸＩＮＧＳＨＡＮＯＦＢＡＮＤＩＲＯＮＦｏＲＭＡＴＩｏＮＳＩＲｏＮＤＥＰＯＳＩＴＩＮＱＩＡＮ’ＡＮＡＲＥＡ，ＨＥＢＥＩＰＲｏＶＩＮＣＥ：Ⅱ訌ＰＬＩＣＡＴＩｏＮＦｏＲＴＨＥＩＲｏＲＩＧＩＮＤＩＮＧＷｅｎ．ｊｕｎｌ’２，ＣＨＥＮＺｈｅｎｇ．１ｅ２，ＣＨＥＮＢｏ．１ｉｎ２，ＤＯＮＧＦａ．ｘｉａｎ２，ＣＵＩＬｉｎｇ—ｌｉｎ９２（１．ＳｃｈｏｏｌｏｆＥａａｈＳｃｉｅｎｃｅｓａｎｄＲｅｓｏｕｒｃｅｓ，ＣｈｉｎａＵｎｉｖｅｒｓｉｔｙｏｆＧｅｏｓｃｉｅｎｃｅｓ（Ｂｅｉｊｉｎｇ），Ｂｅｉｊｉｎｇ１０００８３，Ｃｈｉｎａ；２．ＩｎｓｔｉｔｕｔｅｏｆＧｅｏｍｅｃｈａｎｉｃｓ，ＣｈｉｎｅｓｅＡｃａｄｅｍｙｏｆＧｅｏｌｏｇｉｃａｌＳｃｉｅｎｃｅｓ，Ｂｅｉｊｉｎｇ１０００８１，Ｃｈｉｎａ）Ａｂｓｔｒａｃｔ：ＴｈｅｏｒｉｇｉｎｏｆＱｉａｎ’ａｌｌＢＩＦｓｒｅｍａｉｎｓｕｎｃｌｅａｒ，ａｌｔｈｏｕｇｈｐｌｅｎｔｙｏｆｅｆｆｏｒｔｓｈａｖｅｂｅｅｎｄｏｎｅｉｎｔｈｉｓａｒｅａ（ｅｓｐｅｃｉａｌｌｙｍａｊｏｒａｎｄｏｎｔｈｅＰｒｅｃａｍｂｒｉａｎｇｅｏｌｏｇｙ，ｐｅｔｒｏｌｏｇｙａｎｄｇｅｏｃｈｅｍｉｓｔｒｙ）．Ｉｎｔｈｅｅａｒｌｙｏｒｅｓｓｔａｇｅｏｆ“ＥｘｐｌｏｒｉｎｇＭｉｎｅｓＦａｃｉｎｇＡＲｅｓｏｕｒｓｅｔｒａｃｅＣｒｉｓｉｓ”ｐｒｏｊｅｃｔ，ｌａｒｇｅａｎｄｈｉｇｈ－ｇｒａｄｅｉｒｏｎｎｅｗｗｅｒｅｄｉｓｃｏｖｅｒｅｄ．ＴｈｅｅｌｅｍｅｎｔａｎａｌｙｓｅｓｒｅｐｏｒｔｅｄｉｎｔｈｉｓｐａｐｅｒｐｒｏｖｉｄｅｉｎｓｉｇｈｔｓａｒｅｏｎｔｈｅｏｒｉｇｉｎａｎｄｆｏｒｍａｔｉｏｎｅｎｖｉｒｏｎｍｅｎｔｏｆＱｉａｎ’ａｎＢＩＦｓ．ＴｈｅａｖｅｒａｇｅｂｕｌｋｃｏｍｐｏｓｉｔｉｏｎｓｏｆｔｈｅＢＩＦｓａｒｉｃｈｉｎｔｏｔａｌＦｅａｎｄＳｉ０２，ｃｏｍｐｏｎｅｎｔｉｎｐｕｔ．ＴｈｅｉｒａｎｄｖｅｒｙｌｏｗｉｎＡ１２０３ａｎｄＴｉ０２ｃｏｎｔｅｎｔｓ，ｉｎｄｉｃａｔｉｎｇｔｈａｔｍｉｎｏｒｔｅｒｒｉｇｅｎｏｕｓＰＡＳＳ－ｎｏｒｍａｌｉｚｅｄＲＥＥｐａｔｔｅｒｎｓｓｈｏｗｓｔｒｏｎｇｌｙｅｎｒｉｃｈｅｄＨＲＥＥａｎｄｐｏｓｉｔｉｖｅａｎｏｍａｌｉｅｓｏｆＬａ，ＥｕａｎｄＹ．Ａｌｌｏｆｔｈｅｇｅｏｃｈｅｍｉｓｔｒｙｆｉｎｇｅｒｐｒｉｎｔｓ，ｉｎｃｏｍｂｉｎａｔｉｏｎｗｉｔｈＣｏ／Ｚｎ，Ｎｉ／Ｚｎ，Ｙ／Ｈｏ（＞４４），Ｌａ／Ｌａ。ａｎｄＬａＮ／ＹｂＮ（＜１）ｒａｔｉｏｓ，ｓｔｒｏｎｇｌｙｓｕｇｇｅｓｔａｃｏｍｂｉｎｅｄｏｒｉｇｉｎｏｆａｒｅｎｏｈｙｄｒｏｔｈｅｒｍａｌｗａｔｅｒａｎｄｍａｒｉｎｅｆｏｒＱｉａｎ’ａｎＢＩＦｓ，ｃｏｎｓｉｓｔｅｎｔｗｉｔｈＢＩＦｓｏｔｈｅｒｗｈｅｒｅ．ＴｈｅｒｅｄｉｓｔｉｎｃｔｄｉｆｆｅｒｅｎｃｅｓｂｅｔｗｅｅｎＨｉｇｈ—Ｇｒａｄｅａｎｄｔｒａｃｅｎｏｒｍａｌｔｈａｔｏｒｅｓ，ｗｈｉｃｈｈａｖｅａｐｐａｒｅｎｔｌｙｓｉｍｉｌａｒｏｒｉｇｉｎａｌｓｅｄｉｍｅｎｔａｒｙｂｅｌｔｓ，ｉｎｍａｊｏｒａｎｄｅｌｅｍｅｎｔｃｏｎｔｅｎｔ，ＰＡＳＳ－ｎｏｒｍａｌｉｚｅｄＲＥＥｐａｔｔｅｒｎａｎｄＦｅ－ｂｅａｒｉｎｇｍｉｎｅｒａｌａｓｓｅｍｂｌａｇｅ（ｍａｉｎｌｙｍａｇｎｅｔｉｔｅ），ｄｅｍｏｎｓｔｒａｔｉｎｇｏｒｅｓｔｈｅｙｍｉｇｈｔｈａｖｅｔｈｅｓａｍｅｏｒｉｇｉｎ．Ｉｔｉｓｓｕｇｇｅｓｔｅｄｔｈａｔｔｈｅｈｉｇｈ—ｇｒａｄｅＦｅ—ｒｉｃｈｅｎｖｉｒｏｎｍｅｎｔｄｕｒｉｎｇｖｏｌｃａｎｉｃ－ｓｅｄｉｍｅｎｔａｒｙａｃｔｉｖｉｔｙ．Ｋｅｙｗｏｒｄｓ：ｂａｎｄｉｒｏｎｗｅｒｅｐｒｏｂａｂｌｙｆｏｒｍｅｄａｔｌｏｃａｌｌｙｆｏｒｍａｔｉｏｎｓ（ＢＩＦｓ）；Ｑｉａｎ’ａｎ；ｇｅｏｃｈｅｍｉｓｔｒｙ萬方數(shù)據(jù)河北遷安杏山鐵礦床地球化學特征及其對成礦物質來源的指示作者：作者單位：丁文君，陳正樂，陳柏林，董法先，崔玲玲丁文君(中國地質大學(北京地球科學與資源學院,北京,100083;中國地質科學院地質力學研究所,北京,100081，陳正樂,陳柏林,董法先,崔玲玲(中國地質科學院地質力學研究所,北京,100081地質力學學報JOURNALOFGEOMECHANICS2009,15(42次刊名：英文刊名：年，卷(期：被引用次數(shù)：參考文獻(29條1.李鳳月遷安礦區(qū)太古代地質有關幾問題的探討19922.王凱怡;J.Sills;B.F.Windley冀東遷安地區(qū)太古代片麻雜巖的地球化學和演化19903.李鳳月;宋復梅冀東遷安西群含鐵變質巖系中的輝石及其與鐵礦19924.舒航遷西群巖石地球化學特性及地質意義19895.從柏林;李繼亮;張儒瑗冀東遷西-遷安地區(qū)早太古代變質巖系原巖恢復及其地質意義1982(026.KhanR;SharmaS;PatilDTrace,rare-earthelement,andoxygenisotopicsystematicsforthegenesisofbandedironformations:EvidencefromKushtagischistbelt,ArchaeanDharwarCraton,India19967.GnaaneshwarR;NaqviSGeochemistry,depositionalenvironmentandtectonicsettingoftheBIF'softheLateArchaeanChitradurgaSchistBelt,India19958.JacobsenS;PimentelMANdisotopicstudyoftheHamersleyandMichipicotenbandedironformations-ThesourceofREEandFeinArcheanoceans19889.關廣岳風化淋濾型富鐵礦床的地球化學197610.鞠振南;衛(wèi)廣遠;劉鳳英遼陽弓長嶺富鐵礦的成因探討[期刊論文]-黑龍江科技信息2009(1611.趙斌;李統(tǒng)錦鞍山弓長嶺富磁鐵礦床的形成機制和物理化學條件研究[期刊論文]-地球化學198012.FrancoP;LeonBAreviewofAustralia'sProterozoicmineralsystemsandgeneticmodels200813.李志紅;朱祥坤;唐索寒鞍山--本溪地區(qū)條帶狀鐵建造的鐵同位素與稀土元素特征及其對成礦物質來源的指示[期刊論文]-巖石礦物學雜志2008(0414.NozakiY;ZhangJ;AmakawaHThefractionationbetweenYandHointhemarineenvironment199715.DanielsonA;MllerP;DulskiPTheeuropiumanomaliesinbandedironformationsandthethermalhistoryoftheoceaniccrust199216.KatoY;KawakamiT;KanoTRare-earthelementgeochemistryofbandedironformationsandassociatedamphibolitefromtheSargurbelts,southIndia199617.BauM;DulskiPComparingyttriumandrareearthsinhydrothermalfluidsfromtheMid-AtlanticRidge:implicationsforYandREEbehaviourduringnear-ventmixingandfortheY/HoratioofProterozoicseawater199918.AliboD;NozakiYRareearthelementsinseawater:Particleassociation,shale-normalization,andCeoxidation199919.BanM;MilerP;DulskiPYttriumandlanthanidesineasternMediterraneanseawaterandtheirfractionationduringredox-cycling199720.CampbellA;PalmerM;KlinkhammerGChemistryofhotspringsontheMid-AtlanticRidge198821.McLonnanSRareearthelementsinsedimentaryrocks;influenceofprovenanceandsedimentaryprocesses198922.SugitaniKGeochemicalcharacteristicofArcheanchertsandothersedimentaryrocksinthePilbaraBlock,WesternAustralia:EvidencefortheAreheansea-waterenrichedinhydrothermally-derivedironandsilica199223.RajuPPetrographyandgeochemicalbehaviouroftraceelement,REEandpreciousmetalsignaturesofsulphidicbandedironformationsfromtheChikkasiddavanahalliarea,Chitradurgaschistbelt,India200924.DymekR;KleinCChemistry,p