长江中下游成矿带古元古代董岭片麻岩的锆石U-Pb定年及其地质意义
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摘要
为深入研究长江中下游成矿带基底物质组成和早期构造演化特征,对安徽洪镇地区董岭杂岩中的一套正变质岩系中的黑云母二长片麻岩进行了LA-ICP-MS锆石U-Pb年代学和Lu-Hf同位素研究。结果表明,黑云母二长片麻岩形成于1840Ma,进一步证实长江中下游成矿带存在可靠的古元古代岩浆事件;样品具较低的ε_(Hf)(t)值(-7.2~-12.0),二阶段Hf模式年龄为2.93~3.27 Ga。结合区域研究成果认为,所研究的黑云母二长片麻岩与董岭杂岩中已发现的花岗质正片麻岩(1850 Ma)一样,可能都起源于太古代陆壳物质的再造,形成于与Columbia超大陆的裂解有关的板内伸展-拉张的构造环境,同时还可能参与了该成矿带中中生代的成岩成矿作用。
In order to constrain the basement composition and Paleoproterozoic tectonic evolution of the middle-lower Yangtze metallogenic belt,orthometamorphite( biotite monzonitic gneiss) of the Dongling complex in Hongzhen area,Anhui province was performed zircon U-Pb and Hf isotopic analyses. LA-ICP-MS zircon U-Pb dating yields a ~(206)Pb/207 Pb age of 1. 84 Ga,indicative of the activity of Paleoproterozoic magmatism. Zircons from the gneisses have ε_(Hf)( t) values ranging from-7. 2 to-12. 0 and t_(DM2) model ages from 2. 93 to 3. 27 Ga. Combined with the results of previous studies,we suggest that the biotite monzonitic gneiss and granitic orthogneiss( 1850 Ma) of the Dongling complex were generated by the partial melting of Archean crust in an intraplate extensional setting,which might respond to the breakup of Columbia. In addition,the Precambrian basement has been the major source of widespread Mesozoic magmatism that has been responsible for large-scale Cu-Fe-Au mineralization in the middle-lower Yangtze metallogenic belt.
In order to constrain the basement composition and Paleoproterozoic tectonic evolution of the middle-lower Yangtze metallogenic belt,orthometamorphite( biotite monzonitic gneiss) of the Dongling complex in Hongzhen area,Anhui province was performed zircon U-Pb and Hf isotopic analyses. LA-ICP-MS zircon U-Pb dating yields a ~(206)Pb/207 Pb age of 1. 84 Ga,indicative of the activity of Paleoproterozoic magmatism. Zircons from the gneisses have ε_(Hf)( t) values ranging from-7. 2 to-12. 0 and t_(DM2) model ages from 2. 93 to 3. 27 Ga. Combined with the results of previous studies,we suggest that the biotite monzonitic gneiss and granitic orthogneiss( 1850 Ma) of the Dongling complex were generated by the partial melting of Archean crust in an intraplate extensional setting,which might respond to the breakup of Columbia. In addition,the Precambrian basement has been the major source of widespread Mesozoic magmatism that has been responsible for large-scale Cu-Fe-Au mineralization in the middle-lower Yangtze metallogenic belt.
引文
Andersen T.2002.Correction of common lead in U-Pb analyses that do not report204Pb.Chemical Geology,192(1-2):59-79
Blichert-Toft J,Albarède F.1997.The Lu-Hf geochemistry of chondrites and the evolution of the mantle-crust system.Earth and Planetary Science Letters,148(1-2):243-258
Chen J F,Jahn B M.1998.Crustal evolution of southeastern China:Nd and Sr isotopic evidence.Tectonophysics,284(1-2):101-133
Chen Z H,Xing G F.2016.Geochemical and zircon U-Pb-Hf-O isotopic evidence for a coherent Paleoproterozoic basement beneath the Yangtze Block,South China.Precambrian Research,279:81-90
Gao S,Ling W L,Qiu Y M,Zhou L,Hartmann G,Simon K.1999.Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze craton:Evidence for cratonic evolution and redistribution of REEduring crustal anatexis.Geochimica et Cosmochimica Acta,63(13-14):2071-2088
Gao S,Yang J,Zhou L,Li M,Hu Z C,Guo J L,Yuan H L,Gong HJ,Xiao G Q,Wei J Q.2011.Age and growth of the Archean Kongling terrane,South China,with emphasis on 3.3 Ga granitoid gneisses.American Journal of Science,311(2):153-182
Greentree M R,Li Z X.2008.The oldest known rocks in south-western China:SHRIMP U-Pb magmatic crystallisation age and detrital provenance analysis of the Paleoproterozoic Dahongshan Group.Journal of Asian Earth Sciences,33(5-6):289-302
Griffin W L,Pearson N J,Elusive E,Jackson S E,Van Achterbergh E,O'Reilly S Y,She S R.2000.The Hf isotope composition of crabonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Griffin W L,Wang X,Jackson S E,Pearson N J,O'Reilly S Y,Xu XS,Zhou X M.2002.Zircon chemistry and magma mixing,SEChina:In-situ analysis of Hf isotopes.Tonglu and Pingtan igneous complexes.Lithos,61(3-4):237-269
Grimmer J C,Ratschbacher L,Mc Williams M,Franz L,Gaitzsch I,Tichomorowa M,Hacker B R,Zhang Y Q.2003.When did the ultrahigh-pressure rocks reach the surface?A207Pb/206Pb zircon,40Ar/39Ar white mica,Si-in white mica,single-grain provenance study of Dabie Shan synorogenic foreland sediments.Chemical Geology,197(1-4):87-110
Jiao W F,Wu Y B,Yang S H,Peng M,Wang J.2009.The oldest basement rock in the Yangtze Craton revealed by zircon U-Pb age and Hf isotope composition.Science in China Series D:Earth Sciences,52(9):1393-1399
Li J W,Zhao X F,Zhou M F,Ma C Q,De Souza Z S,Vasconcelos P.2009.Late Mesozoic magmatism from the Daye region,Eastern China:U-Pb ages,petrogenesis,and geodynamic implications.Contributions to Mineralogy and Petrology,157(3):383-409
Li X H,Li W X,Wang X C,Li Q L,Liu Y,Tang G Q,Gao Y Y,Wu F Y.2010.SIMS U-Pb zircon geochronology of porphyry Cu-Au-(Mo)deposits in the Yangtze River Metallogenic Belt,eastern China:Magmatic response to early Cretaceous lithospheric extension.Lithos,119(3-4):427-438
Liu Y S,Hu Z C,Gao S,Günther D,Xu J,Gao C G,Chen H H.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Liu Y S,Gao S,Hu Z C,Gao C G,Zong K Q,Wang D B.2010.Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating,Hf isotopes and trace elements in zircons from mantle xenoliths.Journal of Petrology,51(1-2):537-571
Ludwig K R.2001.ISOPLOT 2.49:A geochronological toolkit for microsoft excel.Berkeley Geochronology Centre:Special Publication,1:1-58
Mao J W,Wang Y T,Lehmann B,Yu J J,Du A D,Mei Y X,Li Y F,Zang W S,Stein H J,Zhou T F.2006.Molybdenite Re-Os and albite40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systems in the Yangtze River valley and metallogenic implications.Ore Geology Reviews,29(3-4):307-324
Pan Y M,Dong P.1999.The lower Changjiang(Yangzi/Yangtze River)metallogenic belt,East Central China:Instrusin-And Wall Rockhosted Cu-Fe-Au,Mo,Zn,Pb,Ag deposits.Ore Geology Reviews,15(4):177-242
Peng M,Wu Y B,Wang J,Jiao W F,Liu X C,Yang S H.2009.Paleoproterozoic mafic dyke from Kongling terrain in the Yangtze Craton and its implication.Chinese Science Bulletin,54(6):1098-1104
Qiu Y M,Gao S,Mc Naughton N J,Groves D I,Ling W L.2000.First evidence of>3.2 Ga continental crust in the Yangtze craton of south China and its implications for Archean crustal evolution and Phanerozoic tectonics.Geology,28(1):11-14
Scherer E,Münker C,Mezger K.2001.Calibration of the lutetium-hafnium clock.Science,293(5530):683-687
Sun M,Chen N S,Zhao G C,Wilde S M,Ye K,Guo J H,Chen Y,Yuan C.2008.U-Pb Zircon and Sm-Nd isotopic study of the Huangtuling granulite,Dabie-Sulu belt,China:Implication for the Paleoproterozoic tectonic history of the Yangtze Craton.American Journal of Science,308(4):469-483
Wang L J,Yu J H,Griffin W L,O'Reilly S Y.2012.Early crustal evolution in the western Yangtze Block:Evidence from U-Pb and Lu-Hf isotopes on detrital zircons from sedimentary rocks.Precambrian Research,222-223:368-385
Wu Y B,Zheng Y F.2004.Genesis of zircon and its constraints on interpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Wu Y B,Zheng Y F,Gao S,Jiao W F,Liu Y S.2008.Zircon U-Pb age and trace element evidence for Paleoproterozoic granulite-facies metamorphism and Archean crustal rocks in the Dabie Orogen.Lithos,101(3-4):308-322
Wu Y B,Gao S,Gong H J,Xiang H,Jiao W F,Yang S H,Liu Y S,Yuan H L.2009.Zircon U-Pb age,trace element and Hf isotope composition of Kongling terrane in the Yangtze Craton:Refining the timing of Palaeoproterozoic high-grade metamorphism.Journal of Metamorphic Geology,27(6):461-477
Wu,Y B,Gao S,Zhang H F,Zheng J P,Liu X C,Wang H,Gong HJ,Zhou L,Yuan H L.2012.Geochemistry and zircon U-Pb geochronology of Paleoproterozoic arc related granitoids in the Northwestern Yangtze Block and its geological implications.Precambrian Research,200-203,26-37
Xiong Q,Zheng J P,Yu C M,Su Y P,Tang H Y,Zhang Z H.2008.Zircon U-Pb age and Hf isotope of Quanyishang A-type granite in Yichang:Significantion for the Yangtze continental cratonization in Paleoproterozoic.Chinese Science Bulletin,54(3):436-446
Yin C Q,Lin S F,Davis D W,Zhao G C,Xiao W J,Li L M,He Y H.2013.2.1-1.85 Ga tectonic events in the Yangtze Block,South China:Petrological and geochronological evidence from the Kongling Complex and implications for the reconstruction of supercontinent Columbia.Lithos,182-183:200-210
Zhang L J,Ma C Q,Wang L X,She Z B,Wang S M.2011.Discovery of Paleoproterozoic rapakivi granite on the northern margin of the Yangtze block and its geological significance.Chinese Science Bulletin,56(3):306-318
Zhang S B,Zheng Y F,Wu Y B,Zhao Z F,Gao S,Wu F Y.2006a.Zircon isotope evidence for≥3.5 Ga continental crust in the Yangtze craton of China.Precambrian Research,146(1-2):16-34
Zhang S B,Zheng Y F,Wu Y B,Zhao Z F,Gao S,Wu F Y.2006b.Zircon U-Pb age and Hf isotope evidence for 3.8 Ga crustal remnant and episodic reworking of Archean crust in South China.Earth and Planetary Science Letters,252(1-2):56-71
Zhang S B,Zheng Y F,Wu Y B,Zhao Z F,Gao S,Wu F Y.2006c.Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic metamorphic event in South China.Precambrian Research,151(3-4):265-288
Zhang S B,He Q,Zheng Y F.2015.Geochronological and geochemical evidence for the nature of the Dongling Complex in South China.Precambrian Research,256:17-30
Zhao X F,Zhou M F,Li J W,Sun M,Gao J F,Sun W H,Yang J H.2010.Late paleoproterozoic to early mesoproterozoic Dongchuan Group in Yunnan,SW China:Implications for tectonic evolution of the Yangtze Block.Precambrian Research,182(1-2):57-69
Zheng J P,Griffin W L,O'Reilly S Y,Zhang M,Pearson N.2006.Zircons in mantle xenoliths record the Triassic Yangtze-North China continental collision.Earth and Planetary Science Letters,247(1-2):130-142
Zheng Y F,Zhang S B.2007.Formation and evolution of Precambrian continental crust in South China.Chinese Science Bulletin,52(1):1-12
Zhu G,Liang C L,Hu B W,Wang Z Q,Wang Y S,Li X.2007.Genesis mechanism of the Hongzhen metamorphic core complex and its tectonic implications.Science in China Series D:Earth Sciences,50(5):649-659
常印佛,刘湘培,吴言昌.1991.长江中下游铜铁成矿带.北京:地质出版社
常印佛,董树文,黄德志.1996.论中-下扬子“一盖多底”格局与演化.资源调查与环境,17(1-2):1-15
邓晋福,戴圣潜,赵海玲,杜建国.2002.铜陵Cu-Au(Ag)成矿区岩浆流体-成矿系统和亚系统的识别.矿床地质,21(4):317-322
董树文,何大林,石永红.1993.安徽董岭花岗岩类的构造特征及侵位机制.地质科学,28(1):10-20,106
董树文,马立成,刘刚,薛怀民,施炜,李建华.2011.论长江中下游成矿动力学.地质学报,85(5):612-625
胡劲平,蒋少涌.2010.宁芜盆地浅成侵入岩的锆石U-Pb年代学和Hf同位素研究及其地质意义.高校地质学报,16(3):294-308
李德威.1993.洪镇变质核杂岩及其成矿意义.大地构造与成矿学,17(3):211-220
李亮,蒋少涌.2009.长江中下游地区九瑞矿集区邓家山花岗闪长斑岩的地球化学与成因研究.岩石学报,25(11):2878-2888
李献华.1996.Sm-Nd模式年龄和等时线年龄的适用性与局限性.地质科学,31(1):97-104
凌文黎.1996.扬子克拉通北缘元古宙基底同位素地质年代学和地壳增生历史:Ⅰ后河群和西乡群.地球科学,21(5):491-494
马振东,蒋敬业,李艳霞,单光祥.1999.长江中下游及邻区基底地球化学分区及区域成矿远景预测.地球科学-中国地质大学学报,24(3):287-291
宁芜玢岩铁矿编写小组.1978.宁芜玢岩铁矿.北京:地质出版社
王丽娟,黄建平,于津海,Griffin W L,王汝城,张少琴,杨颍鹤.2014.长江中下游溧水盆地中基性次火山岩-侵入岩的锆石U-Pb定年和Lu-Hf同位素.科学通报,59(14):1305-1317
王彦斌,刘敦一,曾普胜,杨竹森,蒙义峰,田世洪.2004.铜陵地区小铜官山石英闪长岩锆石SHRIMP的U-Pb年龄及其成因指示.岩石矿物学杂志,23(4):298-304
吴才来,高前明,国和平,郭祥炎,刘良根,郜源红,雷敏,秦海鹏.2010.铜陵中酸性侵入岩成因及锆石SHRIMP定年.岩石学报,26(9):2630-2652
吴淦国,张达,狄永军,臧文拴,张祥信,宋彪,张忠义.2008.铜陵矿集区侵入岩SHRIMP锆石U-Pb年龄及其深部动力学背景.中国科学(D辑),38(5):630-645
谢桂青,毛景文,李瑞玲,张祖送,赵维超,屈文俊,赵财胜,魏世昆.2006.鄂东南地区Cu-Au-Mo-(W)矿床的成矿时代及其成矿地球动力学背景探讨:辉钼矿Re-Os同位素年龄.矿床地质,25(1):43-52
邢凤鸣,徐祥,李志昌.1993.长江中下游早元古代基底的发现及意义.科学通报,38(20):1883-1886
邢凤鸣,徐祥.1995.安徽沿江地区中生代岩浆岩的基本特点.岩石学报,11(4):409-422
徐晓春,陆三明,谢巧勤,楼金伟,褚平利.2008.安徽铜陵冬瓜山铜金矿床流体包裹体微量元素地球化学特征及其地质意义.岩石学报,24(8):1865-1874
翟裕生,姚书振,林新多.1992.长江中下游地区铁铜(金)成矿规律.北京:地质出版社
张旗,简平,刘敦一,王元龙,钱青,王焰,薛怀民.2003.宁芜火山岩的锆石SHRIMP定年及其意义.中国科学(D辑),33(4):309-314
周涛发,范裕,袁峰.2008.长江中下游成矿带成岩成矿作用研究进展.岩石学报,24(8):1665-1678
周涛发,范裕,袁峰,张乐骏,马良,钱兵,谢杰.2011.长江中下游成矿带火山岩盆地的成岩成矿作用.地质学报,85(5):712-730
闫峻,彭戈,初晓强,陈志洪,刘晓强.2011.下扬子洪镇复合岩体:同期多源岩浆作用.全国岩石学与地球动力学论文摘要集(兰州),92
闫峻,彭戈,刘建敏,李全忠,陈志洪,史磊,刘晓强,姜子朝.2012.下扬子繁昌地区花岗岩成因:锆石年代学和Hf-O同位素制约.岩石学报,28(10):3209-3227
Blichert-Toft J,Albarède F.1997.The Lu-Hf geochemistry of chondrites and the evolution of the mantle-crust system.Earth and Planetary Science Letters,148(1-2):243-258
Chen J F,Jahn B M.1998.Crustal evolution of southeastern China:Nd and Sr isotopic evidence.Tectonophysics,284(1-2):101-133
Chen Z H,Xing G F.2016.Geochemical and zircon U-Pb-Hf-O isotopic evidence for a coherent Paleoproterozoic basement beneath the Yangtze Block,South China.Precambrian Research,279:81-90
Gao S,Ling W L,Qiu Y M,Zhou L,Hartmann G,Simon K.1999.Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze craton:Evidence for cratonic evolution and redistribution of REEduring crustal anatexis.Geochimica et Cosmochimica Acta,63(13-14):2071-2088
Gao S,Yang J,Zhou L,Li M,Hu Z C,Guo J L,Yuan H L,Gong HJ,Xiao G Q,Wei J Q.2011.Age and growth of the Archean Kongling terrane,South China,with emphasis on 3.3 Ga granitoid gneisses.American Journal of Science,311(2):153-182
Greentree M R,Li Z X.2008.The oldest known rocks in south-western China:SHRIMP U-Pb magmatic crystallisation age and detrital provenance analysis of the Paleoproterozoic Dahongshan Group.Journal of Asian Earth Sciences,33(5-6):289-302
Griffin W L,Pearson N J,Elusive E,Jackson S E,Van Achterbergh E,O'Reilly S Y,She S R.2000.The Hf isotope composition of crabonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites.Geochimica et Cosmochimica Acta,64(1):133-147
Griffin W L,Wang X,Jackson S E,Pearson N J,O'Reilly S Y,Xu XS,Zhou X M.2002.Zircon chemistry and magma mixing,SEChina:In-situ analysis of Hf isotopes.Tonglu and Pingtan igneous complexes.Lithos,61(3-4):237-269
Grimmer J C,Ratschbacher L,Mc Williams M,Franz L,Gaitzsch I,Tichomorowa M,Hacker B R,Zhang Y Q.2003.When did the ultrahigh-pressure rocks reach the surface?A207Pb/206Pb zircon,40Ar/39Ar white mica,Si-in white mica,single-grain provenance study of Dabie Shan synorogenic foreland sediments.Chemical Geology,197(1-4):87-110
Jiao W F,Wu Y B,Yang S H,Peng M,Wang J.2009.The oldest basement rock in the Yangtze Craton revealed by zircon U-Pb age and Hf isotope composition.Science in China Series D:Earth Sciences,52(9):1393-1399
Li J W,Zhao X F,Zhou M F,Ma C Q,De Souza Z S,Vasconcelos P.2009.Late Mesozoic magmatism from the Daye region,Eastern China:U-Pb ages,petrogenesis,and geodynamic implications.Contributions to Mineralogy and Petrology,157(3):383-409
Li X H,Li W X,Wang X C,Li Q L,Liu Y,Tang G Q,Gao Y Y,Wu F Y.2010.SIMS U-Pb zircon geochronology of porphyry Cu-Au-(Mo)deposits in the Yangtze River Metallogenic Belt,eastern China:Magmatic response to early Cretaceous lithospheric extension.Lithos,119(3-4):427-438
Liu Y S,Hu Z C,Gao S,Günther D,Xu J,Gao C G,Chen H H.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Liu Y S,Gao S,Hu Z C,Gao C G,Zong K Q,Wang D B.2010.Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating,Hf isotopes and trace elements in zircons from mantle xenoliths.Journal of Petrology,51(1-2):537-571
Ludwig K R.2001.ISOPLOT 2.49:A geochronological toolkit for microsoft excel.Berkeley Geochronology Centre:Special Publication,1:1-58
Mao J W,Wang Y T,Lehmann B,Yu J J,Du A D,Mei Y X,Li Y F,Zang W S,Stein H J,Zhou T F.2006.Molybdenite Re-Os and albite40Ar/39Ar dating of Cu-Au-Mo and magnetite porphyry systems in the Yangtze River valley and metallogenic implications.Ore Geology Reviews,29(3-4):307-324
Pan Y M,Dong P.1999.The lower Changjiang(Yangzi/Yangtze River)metallogenic belt,East Central China:Instrusin-And Wall Rockhosted Cu-Fe-Au,Mo,Zn,Pb,Ag deposits.Ore Geology Reviews,15(4):177-242
Peng M,Wu Y B,Wang J,Jiao W F,Liu X C,Yang S H.2009.Paleoproterozoic mafic dyke from Kongling terrain in the Yangtze Craton and its implication.Chinese Science Bulletin,54(6):1098-1104
Qiu Y M,Gao S,Mc Naughton N J,Groves D I,Ling W L.2000.First evidence of>3.2 Ga continental crust in the Yangtze craton of south China and its implications for Archean crustal evolution and Phanerozoic tectonics.Geology,28(1):11-14
Scherer E,Münker C,Mezger K.2001.Calibration of the lutetium-hafnium clock.Science,293(5530):683-687
Sun M,Chen N S,Zhao G C,Wilde S M,Ye K,Guo J H,Chen Y,Yuan C.2008.U-Pb Zircon and Sm-Nd isotopic study of the Huangtuling granulite,Dabie-Sulu belt,China:Implication for the Paleoproterozoic tectonic history of the Yangtze Craton.American Journal of Science,308(4):469-483
Wang L J,Yu J H,Griffin W L,O'Reilly S Y.2012.Early crustal evolution in the western Yangtze Block:Evidence from U-Pb and Lu-Hf isotopes on detrital zircons from sedimentary rocks.Precambrian Research,222-223:368-385
Wu Y B,Zheng Y F.2004.Genesis of zircon and its constraints on interpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Wu Y B,Zheng Y F,Gao S,Jiao W F,Liu Y S.2008.Zircon U-Pb age and trace element evidence for Paleoproterozoic granulite-facies metamorphism and Archean crustal rocks in the Dabie Orogen.Lithos,101(3-4):308-322
Wu Y B,Gao S,Gong H J,Xiang H,Jiao W F,Yang S H,Liu Y S,Yuan H L.2009.Zircon U-Pb age,trace element and Hf isotope composition of Kongling terrane in the Yangtze Craton:Refining the timing of Palaeoproterozoic high-grade metamorphism.Journal of Metamorphic Geology,27(6):461-477
Wu,Y B,Gao S,Zhang H F,Zheng J P,Liu X C,Wang H,Gong HJ,Zhou L,Yuan H L.2012.Geochemistry and zircon U-Pb geochronology of Paleoproterozoic arc related granitoids in the Northwestern Yangtze Block and its geological implications.Precambrian Research,200-203,26-37
Xiong Q,Zheng J P,Yu C M,Su Y P,Tang H Y,Zhang Z H.2008.Zircon U-Pb age and Hf isotope of Quanyishang A-type granite in Yichang:Significantion for the Yangtze continental cratonization in Paleoproterozoic.Chinese Science Bulletin,54(3):436-446
Yin C Q,Lin S F,Davis D W,Zhao G C,Xiao W J,Li L M,He Y H.2013.2.1-1.85 Ga tectonic events in the Yangtze Block,South China:Petrological and geochronological evidence from the Kongling Complex and implications for the reconstruction of supercontinent Columbia.Lithos,182-183:200-210
Zhang L J,Ma C Q,Wang L X,She Z B,Wang S M.2011.Discovery of Paleoproterozoic rapakivi granite on the northern margin of the Yangtze block and its geological significance.Chinese Science Bulletin,56(3):306-318
Zhang S B,Zheng Y F,Wu Y B,Zhao Z F,Gao S,Wu F Y.2006a.Zircon isotope evidence for≥3.5 Ga continental crust in the Yangtze craton of China.Precambrian Research,146(1-2):16-34
Zhang S B,Zheng Y F,Wu Y B,Zhao Z F,Gao S,Wu F Y.2006b.Zircon U-Pb age and Hf isotope evidence for 3.8 Ga crustal remnant and episodic reworking of Archean crust in South China.Earth and Planetary Science Letters,252(1-2):56-71
Zhang S B,Zheng Y F,Wu Y B,Zhao Z F,Gao S,Wu F Y.2006c.Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic metamorphic event in South China.Precambrian Research,151(3-4):265-288
Zhang S B,He Q,Zheng Y F.2015.Geochronological and geochemical evidence for the nature of the Dongling Complex in South China.Precambrian Research,256:17-30
Zhao X F,Zhou M F,Li J W,Sun M,Gao J F,Sun W H,Yang J H.2010.Late paleoproterozoic to early mesoproterozoic Dongchuan Group in Yunnan,SW China:Implications for tectonic evolution of the Yangtze Block.Precambrian Research,182(1-2):57-69
Zheng J P,Griffin W L,O'Reilly S Y,Zhang M,Pearson N.2006.Zircons in mantle xenoliths record the Triassic Yangtze-North China continental collision.Earth and Planetary Science Letters,247(1-2):130-142
Zheng Y F,Zhang S B.2007.Formation and evolution of Precambrian continental crust in South China.Chinese Science Bulletin,52(1):1-12
Zhu G,Liang C L,Hu B W,Wang Z Q,Wang Y S,Li X.2007.Genesis mechanism of the Hongzhen metamorphic core complex and its tectonic implications.Science in China Series D:Earth Sciences,50(5):649-659
常印佛,刘湘培,吴言昌.1991.长江中下游铜铁成矿带.北京:地质出版社
常印佛,董树文,黄德志.1996.论中-下扬子“一盖多底”格局与演化.资源调查与环境,17(1-2):1-15
邓晋福,戴圣潜,赵海玲,杜建国.2002.铜陵Cu-Au(Ag)成矿区岩浆流体-成矿系统和亚系统的识别.矿床地质,21(4):317-322
董树文,何大林,石永红.1993.安徽董岭花岗岩类的构造特征及侵位机制.地质科学,28(1):10-20,106
董树文,马立成,刘刚,薛怀民,施炜,李建华.2011.论长江中下游成矿动力学.地质学报,85(5):612-625
胡劲平,蒋少涌.2010.宁芜盆地浅成侵入岩的锆石U-Pb年代学和Hf同位素研究及其地质意义.高校地质学报,16(3):294-308
李德威.1993.洪镇变质核杂岩及其成矿意义.大地构造与成矿学,17(3):211-220
李亮,蒋少涌.2009.长江中下游地区九瑞矿集区邓家山花岗闪长斑岩的地球化学与成因研究.岩石学报,25(11):2878-2888
李献华.1996.Sm-Nd模式年龄和等时线年龄的适用性与局限性.地质科学,31(1):97-104
凌文黎.1996.扬子克拉通北缘元古宙基底同位素地质年代学和地壳增生历史:Ⅰ后河群和西乡群.地球科学,21(5):491-494
马振东,蒋敬业,李艳霞,单光祥.1999.长江中下游及邻区基底地球化学分区及区域成矿远景预测.地球科学-中国地质大学学报,24(3):287-291
宁芜玢岩铁矿编写小组.1978.宁芜玢岩铁矿.北京:地质出版社
王丽娟,黄建平,于津海,Griffin W L,王汝城,张少琴,杨颍鹤.2014.长江中下游溧水盆地中基性次火山岩-侵入岩的锆石U-Pb定年和Lu-Hf同位素.科学通报,59(14):1305-1317
王彦斌,刘敦一,曾普胜,杨竹森,蒙义峰,田世洪.2004.铜陵地区小铜官山石英闪长岩锆石SHRIMP的U-Pb年龄及其成因指示.岩石矿物学杂志,23(4):298-304
吴才来,高前明,国和平,郭祥炎,刘良根,郜源红,雷敏,秦海鹏.2010.铜陵中酸性侵入岩成因及锆石SHRIMP定年.岩石学报,26(9):2630-2652
吴淦国,张达,狄永军,臧文拴,张祥信,宋彪,张忠义.2008.铜陵矿集区侵入岩SHRIMP锆石U-Pb年龄及其深部动力学背景.中国科学(D辑),38(5):630-645
谢桂青,毛景文,李瑞玲,张祖送,赵维超,屈文俊,赵财胜,魏世昆.2006.鄂东南地区Cu-Au-Mo-(W)矿床的成矿时代及其成矿地球动力学背景探讨:辉钼矿Re-Os同位素年龄.矿床地质,25(1):43-52
邢凤鸣,徐祥,李志昌.1993.长江中下游早元古代基底的发现及意义.科学通报,38(20):1883-1886
邢凤鸣,徐祥.1995.安徽沿江地区中生代岩浆岩的基本特点.岩石学报,11(4):409-422
徐晓春,陆三明,谢巧勤,楼金伟,褚平利.2008.安徽铜陵冬瓜山铜金矿床流体包裹体微量元素地球化学特征及其地质意义.岩石学报,24(8):1865-1874
翟裕生,姚书振,林新多.1992.长江中下游地区铁铜(金)成矿规律.北京:地质出版社
张旗,简平,刘敦一,王元龙,钱青,王焰,薛怀民.2003.宁芜火山岩的锆石SHRIMP定年及其意义.中国科学(D辑),33(4):309-314
周涛发,范裕,袁峰.2008.长江中下游成矿带成岩成矿作用研究进展.岩石学报,24(8):1665-1678
周涛发,范裕,袁峰,张乐骏,马良,钱兵,谢杰.2011.长江中下游成矿带火山岩盆地的成岩成矿作用.地质学报,85(5):712-730
闫峻,彭戈,初晓强,陈志洪,刘晓强.2011.下扬子洪镇复合岩体:同期多源岩浆作用.全国岩石学与地球动力学论文摘要集(兰州),92
闫峻,彭戈,刘建敏,李全忠,陈志洪,史磊,刘晓强,姜子朝.2012.下扬子繁昌地区花岗岩成因:锆石年代学和Hf-O同位素制约.岩石学报,28(10):3209-3227