河北矾山超镁铁岩-正长岩杂岩体中黑云母的特征及其成岩指示意义
|
摘要
河北矾山超镁铁岩一正长岩杂岩体侵位于华北克拉通北缘,为硅不饱和过钾质碱性岩,起源于受古亚洲洋俯冲物质改造过的富集岩石圈地幔。矾山杂岩体侵位于晚三叠世,是华北克拉通北缘三叠纪碱性岩带的代表性岩体之一。本文利用电子探针(EMPA)和激光等离子质谱仪(LA-ICPMS)获得了该特殊岩浆体系下黑云母的主量和微量元素组成,并讨论了其成岩指示意义。矾山杂岩体各类型岩石中的云母均为黑云母,Fe/(Fe+Mg)为0.32~0.57,∑Al为1.179~1.375。黑云母成分记录石榴石辉石正长岩结晶时体系氧逸度LogfO_2=-12.5~-15,温度为680~780℃。矾山杂岩体的黑云母具有极低的稀土元素含量(小于0.100×10~(-6)~1.077×10~(-6)),对全岩稀土元素配分型式基本上没有影响。在微量元素组成上,黑云母是元素Rb、Ba、Nb、Ta、V、Cr、co和Ni的主要载体,其Sr、Zr、Hf、Y、Sc、Th和U的含量明显低于全岩。黑云母成分反映矾山杂岩体岩浆体系以富Fe、高氧逸度为特征,这可能是该杂岩体发育具有经济价值铁矿床的原因之一。
The Fanshan ultramafic-syenitic complex is located on the northern margin of North China Craton(NCC),and crystallized from a SiO_2-undersaturated ultrapotassic alkaline-peralkaline parent magma which was originated from an enriched lithospheric mantle source that had previously been metasomatized by melts from carbonated oceanic crust above a subduction zone.The Fanshan complex was emplaced in late Trassic,and is a typical compelx among the alkaline/ultramafic magmatic belt along the northern margin of NCC.Major and trace elements compositions of biotites from the Fanshan complex are obtained using electron microprobe(EMPA) and laser ablation inductively coupled plasma mass spectrometry(LAICPMS),respectively.The biotites from the Fanshan complex have Fe/(Fe + Mg) in the range 0.32 ~0.57,and total Al from 1.179 to 1.375,and belong to typical biotite.Biotite compositions indicate that the crystallization temperatures of the garnet-clinopyroxene syenites are between 680℃ and 780℃,and their oxygen fugacity(fO_2) = 10~(-12.5) ~10~(-15).The biotites from the Fanshan complex have relatively low contents of rare-earth elements(REE) with total REE contents lower than 0.100 × 10~(-6) ~1.077 × 10~(-6),indicating that biotite is not a major carrier of REE of the whole rock.However,trace elements compositions of biotites indicate that biotite is a major carrier of Rb,Ba,Nb,Ta,V,Cr,Co and Ni;whereas the contents of Sr,Zr,Hf,Y,Sc,Th and U of biotites are much lower than those of whole rock.Biotite compositions suggest that the Fanshan complex is characterized by high Fe contents and high oxygen fugacity,which may be the reason why the complex hosts an apatite-magnetite deposit.
The Fanshan ultramafic-syenitic complex is located on the northern margin of North China Craton(NCC),and crystallized from a SiO_2-undersaturated ultrapotassic alkaline-peralkaline parent magma which was originated from an enriched lithospheric mantle source that had previously been metasomatized by melts from carbonated oceanic crust above a subduction zone.The Fanshan complex was emplaced in late Trassic,and is a typical compelx among the alkaline/ultramafic magmatic belt along the northern margin of NCC.Major and trace elements compositions of biotites from the Fanshan complex are obtained using electron microprobe(EMPA) and laser ablation inductively coupled plasma mass spectrometry(LAICPMS),respectively.The biotites from the Fanshan complex have Fe/(Fe + Mg) in the range 0.32 ~0.57,and total Al from 1.179 to 1.375,and belong to typical biotite.Biotite compositions indicate that the crystallization temperatures of the garnet-clinopyroxene syenites are between 680℃ and 780℃,and their oxygen fugacity(fO_2) = 10~(-12.5) ~10~(-15).The biotites from the Fanshan complex have relatively low contents of rare-earth elements(REE) with total REE contents lower than 0.100 × 10~(-6) ~1.077 × 10~(-6),indicating that biotite is not a major carrier of REE of the whole rock.However,trace elements compositions of biotites indicate that biotite is a major carrier of Rb,Ba,Nb,Ta,V,Cr,Co and Ni;whereas the contents of Sr,Zr,Hf,Y,Sc,Th and U of biotites are much lower than those of whole rock.Biotite compositions suggest that the Fanshan complex is characterized by high Fe contents and high oxygen fugacity,which may be the reason why the complex hosts an apatite-magnetite deposit.
引文
胡建,邱检生,王汝成,蒋少勇,凌洪飞,王孝磊.2006.广东龙窝和白石冈岩体锆石U-Pb年代学、黑云母矿物化学及其成岩指示意义.岩石学报,22(1 0):2464~2474.
李鸿莉,毕献武,胡瑞忠,彭建堂,双燕,李兆丽,李晓敏,袁顺达.2007.芙蓉锡矿田骑田岭花岗岩黑云母矿物化学组成及其对锡成矿的指示意义.岩石学报,23(10):2605~2614.
刘彬,马昌前,刘园园,熊富浩.2010.鄂东南铜山口铜(钼)矿床黑云母矿物化学特征及其对岩石成因与成矿的指示.岩石矿物学杂志,29(2):151~165.
楼亚儿,杜杨松.2006.安徽繁昌-铜陵中生代侵入岩的黑云母特征和成因探讨.矿物学报,26(2):175~180.
牟保垒,阎国翰.1992.燕辽三叠纪碱性偏碱性杂岩体地球化学特征及意义.地质学报,66(2):108~121.
牟保磊,江培谟,曾贻善,阎国翰.1988.矾山杂岩体磷-铁矿床.北京大学出版社,北京,pp.1~15.
牛晓露,陈斌,马旭.2009.河北矾山杂岩体中单斜辉石的研究.岩石学报,25(2):359~373.
任荣,牟保磊,韩宝福,张磊,陈家富,徐钊,宋彪,2009.河北矾山钾质碱性超镁铁岩-正长岩杂岩体的锆石SHRIMP U-Pb年龄.岩石学报,25(3):588~594.
谢应雯,梁华英,张玉泉.2002.藏东及邻区钾玄岩系岩石云母特征及其岩石学意义.岩石学报,18(2):205~211.
谢应雯,张玉泉.1995.哀牢山-金沙江裂谷系岩石中镁铁云母成分特征及其岩石学意义.矿物学报,15(1):82~87.
阎国翰,牟保磊,许保良,何国琦,谭林坤,赵晖,何中甫,张任祜,乔广生.2000.燕辽-阴山三叠纪碱性岩年代学和Sr,Nd,Pb同位素特征及意义.中国科学(D辑),30(4):383~387.
翟明国.2004.华北克拉通2.1~1.7Ga地质事件群的分解和构造意义探讨.岩石学报,20(6):1343~1354.
张遵忠,顾连兴,吴昌志,三金柱,汤晓茜,郗爱华,王硕.2005.东天山尾亚杂岩体:同源还是异源?——来自黑云母的证据.地球化学,34(4):328~338.
周作侠.1988.侵入岩的镁铁云母化学成分特征及其地质意义.岩石学报,3:63~73.
Albuquerque A C.1973.Geochemistry of biotites from granitic rocks,northern Portugal.Geochimica et Cosmochimica Acta,37:1779~1802.
Avanzinelli R,Lustrino M,Mattei M,Melluso L,Conticelli S.2009.Potassic and ultrapotassic magmatism in the circumTyrrhenian region:significance of carbonated pelitic vs.pelitic sediment recycling at destructive plate margins.Lithos,113:213~217.
Ayer J A.1998.The mafic minerals of the Falcon Island ultrapotassic pluton,Lake of the Woods,Ontario:progressive reduction during fractionation.The Canadian Mineralogist,36:49~66.
Boynton W V.1984.Geochemistry of the earth elements:Meteorite studies.In:Henderson P.(Ed.),Rare Earth Element Geochemistry.Elsevier,pp.63~114.
Buddington A F,Lindsley D H.1964.Iron-titanium oxide minerals and synthetic equivalents.Journal of Petrology,5:310~357.
Chen B,Jahn B M,Tian W.2009.Evolution of the Solonker suture zone:constraints from zircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotopic compositions of subduction-and collision-related magmas and forearc sediments.Journal of Asian Earth Sciences,34:245~257.
Chen B,Jahn B M,Wilde S,Xu B.2000.Two contrasting Paleozoic magmatic belts in northern Inner Mongolia,China:petrogenesis and tectonic implications.Tectonophysics,328:157~182.
Cheng C,Sun S H.2003.The Fanshan apatite-magnetite deposit in the potassic ultramafic layered intrusions.North China.Resource Geology,53:163~174.
Conticelli S,Carlson R W,Widom E,Serri G.2007.Chemical and isotopic composition(Os,Pb,Nd,and Sr)of Neogene to Quaternary calc-alkalic,shoshonitic,and ultrapotassic mafic rocks from the Italian peninsula:inferences on the nature of their mantle sources.In:Beccaluva,L.,Bianchini,G.,Wilson,M.(Eds.),Cenozoic Volcanism in the Mediterranean Area.Geological Society of America Special Paper,418,pp.171~202.
Conticelli S,Guarnieri L,Farinelli A,Mattei M,Avanzinelli R,Bianchini G,Boari E,Tommasini S,Tiepolo M,Prelevic D,Venturelli G.2009.Trace elements and Sr-Nd-Pb isotopes of K-rich,shoshonitic,and calc-alkaline magmatism of the Western Mediterranean Region:genesis of ultrapotassic to calcalkaline magmatic associations in a post-collisional geodynamic setting.Lithos,107:68~92.
Feldstein S N,Lange R A.1999.Pliocene potassic magmas from the Kings River Region,Sierra Nevada.California:evidence for melting of a subduction modified mantle.Journal of Petrology,40:1301~1320.
Foley S F,Venturelli G,Green D H,Toscani L.1987.The ultrapotassic rocks:characteristics,classification,and constrains for petrogenenetic models.Earth-Science Reviews,24:81~134.
Jahn B M,Auvray B,Cornichet J,Bai Y L,Shen Q H,Liu D Y.1987.3.5 Ga old amphibolites from eastern Hebei province,China:field occurrence,petrology,Sm-Nd isochron age and REE geochemistry.Precambrian Research,34:311~346.
Jahn B M,Auvray B,Shen QH,Liu D Y,Zhang Z Q,Dong YJ,Ye X J,Zhang Q Z,Cornichet J,Mace J.1988.Archean crustal evolution in China:The Taishan complex,and evidence for juvenile crustal addition from long-term depleted mantle.Precambrian Research,38:381~403.
Jahn B M,Wu F Y,Chen B.2000.Granitoids of the Central Asian Orogenic Belt and continental growth in the Phanerozoic.Transactions of the Royal Society of Edinburgh:Earth Sciences,91:171~184.
Jiang N,Chu X L,Mizuta T,Ishiyama D,Mi J G.2004.A magnetite-apatite deposit in the Fanshan alkaline ultramafic complex,Northern China.Economic Geology,99:397~408.
Lalonde A E,Bernard P.1993.Composition and color of biotite from granites:Two useful properties in the characterization of plutonic suites from the Hepburn internal zone of Wopmay Orogen,Northwest Territories.The Canadian Mineralogist,31:203~217.
Liu D Y,Nutman A P,Compston W,Wu I S,Shen Q H.1992.Remnants of≥3800 Ma crust in the Chinese part of the SinoKorean Craton.Geology,20:339~342.
Miller C,Schuster R,Klotzli U,Frank W,Purtscheller F.1999.Post-collisional potassic and ultrapotassic magmatism in SW Tibet:geochemieal and Sr-Nd-Pb-O isotopic constrains for mantle source characteristics and petrogenesis.Journal of Petrology,40:1399~1424.
Niu X L,Chen B,Liu A K,Suzuki K,Ma X.2012.Petrological and Sr-Nd-Os isotopic constraints on the origin of the Fanshan ultrapotassic complex from the North China Croton.Lithos,149:146-158.
Rieder M,Cavazzini G,D'Yakonov Y S,Frank-Kamenetskii V A,Gottardi G,Guggenheim S,Koval PV,Muller G,Neiva A R,Radoslovich E W,Robbert J L,Sassi F P,Takeda H,Weiss H,Wones D R.1998.Nomenclature of the micas.The Canadian Mineralogist,36:905~912.
Sengor A M C,Natal in B A.1996.Paleotectonics of Asia:fragments of a synthesis.In:Yin,A.,Harrison,T.M.(Eds.),The Tectonic Evolution of Asia.Cambridge University Press,Cambridge,pp.486~641.
Shabani A A T,Lalonde A E,Whalen J B.2003.Composition of biotite from granitic rocks of the Canadian Appalachian orogen:A potential tectonomagmatic indicator?The Canadian Mineralogist,41:1381~1396.
Sun S S,McDonough W F.1989.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes.In:Saunders,A.D.,Norry,M.J.(Eds.),Magmatism in the Ocean Basins.Geological Society,London,Special Publications,42,pp.313~345.
Windley B F,Alexelev D,Xiao W J,Kroner A,Badarch G.2007.Tectonic models for accretion of the Central Asian Orogenic Belt.Journal of the Geological Society,164:31~47.
Wones D R,Eugster H P.1965.Stability of biotite:Experiment,theory,and application.American Mineralogist,50:1228~1272.
Xiao W J,Windley B F,Hao J,Zhai M G.2003.Accretion leading to collision and the Permian solonker suture,Inner Mongolia,China:termination of the Central Asian Orogenic Belt.Tectonics,22,1609,doi:10.1029/2002TC001484.
Yan G H,Mu BL,Xu B L,He G Q,Tan L K,Zhao H,He Z F,Zhang R H,Qiao G S.1999.Triassic alkaline intrusive in the Yanliao-Yinshan area:Their chronology,Sr,Nd and Pb isotopic characteristics and their implication.Science In China(ser.D),42(6):582~587.
Zhang S H,Zhao Y,Kroner A,Liu X M,Xie L W,Chen F K.2009.Early Permian plutons from the northern North China Block:constraints on continental arc evolution and convergent margin magmatism related to the Central Asian Orogenic Belt.International Journal of Earth Science,98:1441~1467.
Zhang S H,Zhao Y,Song B,Liu D Y.2007a.Petrogenesis of the middle Devonian Gushan diorite pluton on the northern margin of the North China block and its tectonic implications.Geological Magazine,144:553~568.
Zhang S H,Zhao Y,Song B,Yang Z Y,Hu J M,Wu H.2007b.Carboniferous granitic plutons from the northern margin of the North China block:implications for a late Paleozoic active continental margin.Journal of the Geological Society,164:451~463.
Zhao G,Sun M,Wilde S A,Sanzhong L,2005.Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited.Precambrian Research,136:177~202.
Zhao Z,Mo X,Dilek Y,Niu Y,DePaolo D J,Robinson P,Zhu D,Sun C,Dong G,Zhou S,Luo Z,Hou Z.2009.Geochemical and Sr-Nd-Pb-O isotopic compositions of the post-collisional ultrapotassic magmatism in SW Tibet:petrogenesis and implications for India intra-continental subduction beneath southern Tibet.Lithos,113:190~212.
李鸿莉,毕献武,胡瑞忠,彭建堂,双燕,李兆丽,李晓敏,袁顺达.2007.芙蓉锡矿田骑田岭花岗岩黑云母矿物化学组成及其对锡成矿的指示意义.岩石学报,23(10):2605~2614.
刘彬,马昌前,刘园园,熊富浩.2010.鄂东南铜山口铜(钼)矿床黑云母矿物化学特征及其对岩石成因与成矿的指示.岩石矿物学杂志,29(2):151~165.
楼亚儿,杜杨松.2006.安徽繁昌-铜陵中生代侵入岩的黑云母特征和成因探讨.矿物学报,26(2):175~180.
牟保垒,阎国翰.1992.燕辽三叠纪碱性偏碱性杂岩体地球化学特征及意义.地质学报,66(2):108~121.
牟保磊,江培谟,曾贻善,阎国翰.1988.矾山杂岩体磷-铁矿床.北京大学出版社,北京,pp.1~15.
牛晓露,陈斌,马旭.2009.河北矾山杂岩体中单斜辉石的研究.岩石学报,25(2):359~373.
任荣,牟保磊,韩宝福,张磊,陈家富,徐钊,宋彪,2009.河北矾山钾质碱性超镁铁岩-正长岩杂岩体的锆石SHRIMP U-Pb年龄.岩石学报,25(3):588~594.
谢应雯,梁华英,张玉泉.2002.藏东及邻区钾玄岩系岩石云母特征及其岩石学意义.岩石学报,18(2):205~211.
谢应雯,张玉泉.1995.哀牢山-金沙江裂谷系岩石中镁铁云母成分特征及其岩石学意义.矿物学报,15(1):82~87.
阎国翰,牟保磊,许保良,何国琦,谭林坤,赵晖,何中甫,张任祜,乔广生.2000.燕辽-阴山三叠纪碱性岩年代学和Sr,Nd,Pb同位素特征及意义.中国科学(D辑),30(4):383~387.
翟明国.2004.华北克拉通2.1~1.7Ga地质事件群的分解和构造意义探讨.岩石学报,20(6):1343~1354.
张遵忠,顾连兴,吴昌志,三金柱,汤晓茜,郗爱华,王硕.2005.东天山尾亚杂岩体:同源还是异源?——来自黑云母的证据.地球化学,34(4):328~338.
周作侠.1988.侵入岩的镁铁云母化学成分特征及其地质意义.岩石学报,3:63~73.
Albuquerque A C.1973.Geochemistry of biotites from granitic rocks,northern Portugal.Geochimica et Cosmochimica Acta,37:1779~1802.
Avanzinelli R,Lustrino M,Mattei M,Melluso L,Conticelli S.2009.Potassic and ultrapotassic magmatism in the circumTyrrhenian region:significance of carbonated pelitic vs.pelitic sediment recycling at destructive plate margins.Lithos,113:213~217.
Ayer J A.1998.The mafic minerals of the Falcon Island ultrapotassic pluton,Lake of the Woods,Ontario:progressive reduction during fractionation.The Canadian Mineralogist,36:49~66.
Boynton W V.1984.Geochemistry of the earth elements:Meteorite studies.In:Henderson P.(Ed.),Rare Earth Element Geochemistry.Elsevier,pp.63~114.
Buddington A F,Lindsley D H.1964.Iron-titanium oxide minerals and synthetic equivalents.Journal of Petrology,5:310~357.
Chen B,Jahn B M,Tian W.2009.Evolution of the Solonker suture zone:constraints from zircon U-Pb ages,Hf isotopic ratios and whole-rock Nd-Sr isotopic compositions of subduction-and collision-related magmas and forearc sediments.Journal of Asian Earth Sciences,34:245~257.
Chen B,Jahn B M,Wilde S,Xu B.2000.Two contrasting Paleozoic magmatic belts in northern Inner Mongolia,China:petrogenesis and tectonic implications.Tectonophysics,328:157~182.
Cheng C,Sun S H.2003.The Fanshan apatite-magnetite deposit in the potassic ultramafic layered intrusions.North China.Resource Geology,53:163~174.
Conticelli S,Carlson R W,Widom E,Serri G.2007.Chemical and isotopic composition(Os,Pb,Nd,and Sr)of Neogene to Quaternary calc-alkalic,shoshonitic,and ultrapotassic mafic rocks from the Italian peninsula:inferences on the nature of their mantle sources.In:Beccaluva,L.,Bianchini,G.,Wilson,M.(Eds.),Cenozoic Volcanism in the Mediterranean Area.Geological Society of America Special Paper,418,pp.171~202.
Conticelli S,Guarnieri L,Farinelli A,Mattei M,Avanzinelli R,Bianchini G,Boari E,Tommasini S,Tiepolo M,Prelevic D,Venturelli G.2009.Trace elements and Sr-Nd-Pb isotopes of K-rich,shoshonitic,and calc-alkaline magmatism of the Western Mediterranean Region:genesis of ultrapotassic to calcalkaline magmatic associations in a post-collisional geodynamic setting.Lithos,107:68~92.
Feldstein S N,Lange R A.1999.Pliocene potassic magmas from the Kings River Region,Sierra Nevada.California:evidence for melting of a subduction modified mantle.Journal of Petrology,40:1301~1320.
Foley S F,Venturelli G,Green D H,Toscani L.1987.The ultrapotassic rocks:characteristics,classification,and constrains for petrogenenetic models.Earth-Science Reviews,24:81~134.
Jahn B M,Auvray B,Cornichet J,Bai Y L,Shen Q H,Liu D Y.1987.3.5 Ga old amphibolites from eastern Hebei province,China:field occurrence,petrology,Sm-Nd isochron age and REE geochemistry.Precambrian Research,34:311~346.
Jahn B M,Auvray B,Shen QH,Liu D Y,Zhang Z Q,Dong YJ,Ye X J,Zhang Q Z,Cornichet J,Mace J.1988.Archean crustal evolution in China:The Taishan complex,and evidence for juvenile crustal addition from long-term depleted mantle.Precambrian Research,38:381~403.
Jahn B M,Wu F Y,Chen B.2000.Granitoids of the Central Asian Orogenic Belt and continental growth in the Phanerozoic.Transactions of the Royal Society of Edinburgh:Earth Sciences,91:171~184.
Jiang N,Chu X L,Mizuta T,Ishiyama D,Mi J G.2004.A magnetite-apatite deposit in the Fanshan alkaline ultramafic complex,Northern China.Economic Geology,99:397~408.
Lalonde A E,Bernard P.1993.Composition and color of biotite from granites:Two useful properties in the characterization of plutonic suites from the Hepburn internal zone of Wopmay Orogen,Northwest Territories.The Canadian Mineralogist,31:203~217.
Liu D Y,Nutman A P,Compston W,Wu I S,Shen Q H.1992.Remnants of≥3800 Ma crust in the Chinese part of the SinoKorean Craton.Geology,20:339~342.
Miller C,Schuster R,Klotzli U,Frank W,Purtscheller F.1999.Post-collisional potassic and ultrapotassic magmatism in SW Tibet:geochemieal and Sr-Nd-Pb-O isotopic constrains for mantle source characteristics and petrogenesis.Journal of Petrology,40:1399~1424.
Niu X L,Chen B,Liu A K,Suzuki K,Ma X.2012.Petrological and Sr-Nd-Os isotopic constraints on the origin of the Fanshan ultrapotassic complex from the North China Croton.Lithos,149:146-158.
Rieder M,Cavazzini G,D'Yakonov Y S,Frank-Kamenetskii V A,Gottardi G,Guggenheim S,Koval PV,Muller G,Neiva A R,Radoslovich E W,Robbert J L,Sassi F P,Takeda H,Weiss H,Wones D R.1998.Nomenclature of the micas.The Canadian Mineralogist,36:905~912.
Sengor A M C,Natal in B A.1996.Paleotectonics of Asia:fragments of a synthesis.In:Yin,A.,Harrison,T.M.(Eds.),The Tectonic Evolution of Asia.Cambridge University Press,Cambridge,pp.486~641.
Shabani A A T,Lalonde A E,Whalen J B.2003.Composition of biotite from granitic rocks of the Canadian Appalachian orogen:A potential tectonomagmatic indicator?The Canadian Mineralogist,41:1381~1396.
Sun S S,McDonough W F.1989.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes.In:Saunders,A.D.,Norry,M.J.(Eds.),Magmatism in the Ocean Basins.Geological Society,London,Special Publications,42,pp.313~345.
Windley B F,Alexelev D,Xiao W J,Kroner A,Badarch G.2007.Tectonic models for accretion of the Central Asian Orogenic Belt.Journal of the Geological Society,164:31~47.
Wones D R,Eugster H P.1965.Stability of biotite:Experiment,theory,and application.American Mineralogist,50:1228~1272.
Xiao W J,Windley B F,Hao J,Zhai M G.2003.Accretion leading to collision and the Permian solonker suture,Inner Mongolia,China:termination of the Central Asian Orogenic Belt.Tectonics,22,1609,doi:10.1029/2002TC001484.
Yan G H,Mu BL,Xu B L,He G Q,Tan L K,Zhao H,He Z F,Zhang R H,Qiao G S.1999.Triassic alkaline intrusive in the Yanliao-Yinshan area:Their chronology,Sr,Nd and Pb isotopic characteristics and their implication.Science In China(ser.D),42(6):582~587.
Zhang S H,Zhao Y,Kroner A,Liu X M,Xie L W,Chen F K.2009.Early Permian plutons from the northern North China Block:constraints on continental arc evolution and convergent margin magmatism related to the Central Asian Orogenic Belt.International Journal of Earth Science,98:1441~1467.
Zhang S H,Zhao Y,Song B,Liu D Y.2007a.Petrogenesis of the middle Devonian Gushan diorite pluton on the northern margin of the North China block and its tectonic implications.Geological Magazine,144:553~568.
Zhang S H,Zhao Y,Song B,Yang Z Y,Hu J M,Wu H.2007b.Carboniferous granitic plutons from the northern margin of the North China block:implications for a late Paleozoic active continental margin.Journal of the Geological Society,164:451~463.
Zhao G,Sun M,Wilde S A,Sanzhong L,2005.Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited.Precambrian Research,136:177~202.
Zhao Z,Mo X,Dilek Y,Niu Y,DePaolo D J,Robinson P,Zhu D,Sun C,Dong G,Zhou S,Luo Z,Hou Z.2009.Geochemical and Sr-Nd-Pb-O isotopic compositions of the post-collisional ultrapotassic magmatism in SW Tibet:petrogenesis and implications for India intra-continental subduction beneath southern Tibet.Lithos,113:190~212.
目录