华北克拉通南缘古元古代末(～1.84Ga)垣头A-型花岗岩成因及其构造意义
|
摘要
在华北克拉通陆续发现有大量的古元古代末-中元古代早期A-型花岗岩,它们具有独特的地球化学特征和特定的形成条件,可为进一步了解A-型花岗岩的岩石成因以及华北克拉通由结晶基底的形成向稳定盖层发育时期构造环境的转折提供重要依据。本文对华北克拉通南缘产出的垣头花岗岩体进行了岩石学、锆石U-Pb年代学、元素地球化学和Nd-Hf-O同位素研究。结果表明,垣头岩体岩石类型主要为正长花岗岩,形成时代为1841±4Ma;全岩样品具有较高的铁(FeO~T/(FeO~T+MgO)=0. 75～0. 86)、富碱(K_2O+Na_2O=8. 11%～9. 13%,K_2O/Na_2O> 1)、低MgO (0. 28%～0. 56%)、P_2O_5(0. 04%～0. 08%)和MnO(0. 03%～0. 04%),富含大离子亲石元素(如Rb、Th、U、K)、亏损高场强元素(Nb、Ta、Zr、Hf),具有Eu、Sr负异常,高10,000Ga/Al比值(> 2. 76)、准铝质-弱过铝质且不含碱性暗色矿物,属于铝质A-型花岗岩;全岩εNd(t)=-4. 68、tC DM=2. 70Ga,锆石εHf(t)=-12. 0～-4. 71、tC8DM=3. 22～2. 78Ga,锆石δ1O=5. 4‰～6. 5‰(加权平均值为6. 1‰),指示它们是古老基底物质部分熔融的产物。结合区域上的地质特征和研究资料,我们认为垣头A-型花岗岩体形成于碰撞后的伸展环境,标志着华北克拉通1. 85Ga前后的造山运动的结束。
The North China Craton( NCC) has been successively recognized many Late Paleoproterozoic to Early Mesoproterozoic Atype granites,showing unique geochemistry characteristics and particular formation environment,which would provide further important insights into their petrogenesis and tectonic transition from the formation of crystalline basement to the deposition of stable sedimentary cover in NCC. Here we report systematic investigation on petrology,geochronology,elemental geochemistry,and Nd-Hf-O isotopic characteristics of the Yuantou pluton in the southern margin of the NCC. The results show that the Yuantou pluton mainly consists of syenogranite,which was emplaced at 1841 ± 4 Ma. All rocks are rich in ferroan( FeO T/( FeO T+ MgO) = 0. 75 ～ 0. 86) and alkaline( K_2O + Na_2O = 8. 11% ～ 9. 13%,K_2O/Na_2O > 1),but poor in MgO( 0. 28% ～ 0. 56%),P_2O_5( 0. 04% ～ 0. 08%) and MnO( 0. 03% ～ 0. 04%). Additionally,they show enrichment of LILEs( Rb,Th,U,K),depletion of HFSEs( Nb,Ta,Zr,Hf) with negative Eu and Sr anomalies. Their high 10,000 Ga/Al ratios( > 2. 76) with metaluminous to peraluminous characteristics,containing biotite without alkali mafic minerals,show an affinity to aluminous A-type granite. The Late Paleoproterozoic A-type granite displays low whole-rock εNd( t) value(-4. 68) with two-stage Nd model age of 2. 70 Ga,low zircon εHf( t) values(-12. 0 ～-4. 71) with zircon two-stage Hf model ages of 3. 22 ～ 2. 78 Ga,and high zircon δ~(18)O values( 5. 4‰ to 6. 5‰,weighted mean = 6. 1‰),indicating that the Yuantou A-type granite was derived predominantly from partial melting of the ancient continental crust. Combined with above results and regional geological data,the Yuantou A-type granite was related to the underplating of mafic magmas in a post-collisional regime,marking the end of ～ 1. 85 Ga orogenic movement in the NCC.
The North China Craton( NCC) has been successively recognized many Late Paleoproterozoic to Early Mesoproterozoic Atype granites,showing unique geochemistry characteristics and particular formation environment,which would provide further important insights into their petrogenesis and tectonic transition from the formation of crystalline basement to the deposition of stable sedimentary cover in NCC. Here we report systematic investigation on petrology,geochronology,elemental geochemistry,and Nd-Hf-O isotopic characteristics of the Yuantou pluton in the southern margin of the NCC. The results show that the Yuantou pluton mainly consists of syenogranite,which was emplaced at 1841 ± 4 Ma. All rocks are rich in ferroan( FeO T/( FeO T+ MgO) = 0. 75 ～ 0. 86) and alkaline( K_2O + Na_2O = 8. 11% ～ 9. 13%,K_2O/Na_2O > 1),but poor in MgO( 0. 28% ～ 0. 56%),P_2O_5( 0. 04% ～ 0. 08%) and MnO( 0. 03% ～ 0. 04%). Additionally,they show enrichment of LILEs( Rb,Th,U,K),depletion of HFSEs( Nb,Ta,Zr,Hf) with negative Eu and Sr anomalies. Their high 10,000 Ga/Al ratios( > 2. 76) with metaluminous to peraluminous characteristics,containing biotite without alkali mafic minerals,show an affinity to aluminous A-type granite. The Late Paleoproterozoic A-type granite displays low whole-rock εNd( t) value(-4. 68) with two-stage Nd model age of 2. 70 Ga,low zircon εHf( t) values(-12. 0 ～-4. 71) with zircon two-stage Hf model ages of 3. 22 ～ 2. 78 Ga,and high zircon δ~(18)O values( 5. 4‰ to 6. 5‰,weighted mean = 6. 1‰),indicating that the Yuantou A-type granite was derived predominantly from partial melting of the ancient continental crust. Combined with above results and regional geological data,the Yuantou A-type granite was related to the underplating of mafic magmas in a post-collisional regime,marking the end of ～ 1. 85 Ga orogenic movement in the NCC.
引文
All China Commission of Stratigraphy.2002.The Instruction Book of Regional Chronostratigraphic(Geological Time)Scale in China.Beijing:Geological Publishing House(in Chinese)
Anderson JL and Bender EE.1989.Nature and origin of Proterozoic A-type granitic magmatism in the southwestern United States of America.Lithos,23(1-2):19-52
Bai J,Huang XG,Wang HC et al.1996.The Precambrian Crustal Evolution of China.Beijing:Geological Publishing House(in Chinese)
Bao ZW,Wang Q,Zi F,Tang GJ,Du FJ and Bai GD.2009.Geochemistry of the Paleoproterozoic Longwangzhuang A-type granites on the southern margin of North China Craton:Petrogenesis and tectonic implications.Geochimica,38(6):509-522(in Chinese with English abstract)
Belousova EA,Griffin WL,O’Reilly SY and Fisher NI.2002.Igneous zircon:Trace element composition as an indicator of source rock type.Contributions to Mineralogy and Petrology,143(5):602-622
Bindeman I.2008.Oxygen isotopes in mantle and crustal magmas as revealed by single crystal analysis.Reviews in Mineralogy and Geochemistry,69(1):445-478
Bonin B.2007.A-type granites and related rocks:Evolution of a concept,problems and prospects.Lithos,97(1-2):1-29
Bureau of Geology and Mineral Resources of Shaanxi Province(BGMRS).1989.Regional Geology of Shaanxi Province.Beijing:Geological Publishing House(in Chinese)
Collins WJ,Beams SD,White AJR and Chappell BW.1982.Nature and origin of A-type granites with particular reference to southeastern Australia.Contributions to Mineralogy and Petrology,80(2):189-200
Creaser RA,Price RC and Wormald RJ.1991.A-type granites revisited:Assessment of a residual-source model.Geology,19(2):163-166
Dall’Agnol R,Frost CD and Rm9 OT.2012.IGCP Project 510“A-type granites and related rocks through time”:Project vita,results,and contribution to granite research.Lithos,151:1-16
Deng XQ,Zhao TP,Peng TP,Gao XY and Bao ZW.2015.Petrogenesis of 1600Ma Maping A-type granite in the southern margin of the North China Craton and its tectonic implications.Acta Petrologica Sinica,31(6):1621-1635(in Chinese with English abstract)
Deng XQ,Zhao TP and Peng TP.2016a.Age and geochemistry of the Early Mesoproterozoic A-type granites in the southern margin of the North China Craton:Constraints on their petrogenesis and tectonic implications.Precambrian Research,283:68-88
Deng XQ,Peng TP and Zhao TP.2016b.Geochronology and geochemistry of the late Paleoproterozoic aluminous A-type granite in the Xiaoqinling area along the southern margin of the North China Craton:Petrogenesis and tectonic implications.Precambrian Research,285:127-146
Diwu CR,Sun Y,Lin CL and Wang HL.2010.LA-(MC)-ICPMS U-Pb zircon geochronology and Lu-Hf isotope compositions of the Taihua Complex on the southern margin of the North China Craton.Chinese Science Bulletin,55(23):2557-2571
Diwu CR,Sun Y,Zhao Y and Lai SC.2014.Early Paleoproterozoic(2.45~2.20Ga)magmatic activity during the period of global magmatic shutdown:Implications for the crustal evolution of the southern North China Craton.Precambrian Research,255:627-640
Eby GN.1990.The A-type granitoids:A review of their occurrence and chemical characteristics and speculations on their petrogenesis.Lithos,26(1-2):115-134
Eby GN.1992.Chemical subdivision of the A-type granitoids:Petrogenetic and tectonic implications.Geology,20(7):641-644
Frost CD,Rm9 OT and Dall’Agnol R.2007.IGCP project 510-A-type granites and related rocks through time.Lithos,97(1-2):Vii-Xiii
Frost CD and Frost BR.2011.On ferroan(A-type)granitoids:Their compositional variability and modes of origin.Journal of Petrology,52(1):39-53
Gao SL,Lin JY and Lu YJ.2013.Formation epoch and its geological implications of Paleoprotozoic A-type granite in Shizuizi of Jingyuan County,Ningxia Province.Acta Petrologica Sinica,29(8):2676-2684(in Chinese with English abstract)
Geng YS,Yang CH and Wan YS.2006.Paleoproterozoic granitic magmatism in the Luliang area,North China Craton:Constraint from isotopic geochronology.Acta Petrologica Sinica,22(2):305-314(in Chinese with English abstract)
Guo B,Zhu LM,Li B,Gong HJ and Wang JQ.2009.Zircon U-Pb age and Hf isotope composition of the Huashan and Heyu granite plutons at the southern margin of North China Craton:Implications for geodynamic setting.Acta Petrologica Sinica,25(2):265-281(in Chinese with English abstract)
Guo JH,Shi X,Bian AG,Xu RH,Zhai MG and Li YG.1999.Pb isotopic composition of feldspar and U-Pb age of zircon from early Proterozoic granite in Sanggan area,North China craton:Metamorphism,crustal melting and tectono-thermal event.Acta Petrologica Sinica,15(2):199-207(in Chinese with English abstract)
Hou GT,Liu YL and Li JH.2006.Evidence for~1.8Ga extension of the eastern Block of the North China Craton from SHRIMP U-Pb dating of mafic dyke swarms in Shandong Province.Journal of Asian Earth Sciences,27(4):392-401
Hu GH,Hu JL,Chen W and Zhao TP.2010.Geochemistry and tectonic setting of the 1.78Ga mafic dyke swarms in the Mt.Zhongtiao and Mt.Song areas,the southern margin of the North China Craton.Acta Petrologica Sinica,26(5):1563-1576(in Chinese with English abstract)
Huang HQ,Li XH,Li WX and Li ZX.2011.Formation of highδ18Ofayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks,southern China.Geology,39(10):903-906
King PL,White AJR,Chappell BW and Allen CM.1997.Characterization and origin of aluminous A-type granites from the Lachlan Fold Belt,southeastern Australia.Journal of Petrology,38(3):371-391
Li XH,Liu Y,Li QL,Guo CH and Chamberlain KR.2009.Precise determination of Phanerozoic zircon Pb/Pb age by multicollector SIMS without external standardization.Geochemistry,Geophysics,Geosystems,10(4):Q04010
Liu JH,Liu FL,Ding ZJ,Liu PH,Guo CL and Wang F.2014.Geochronology,petrogenesis and tectonic implications of Paleoproterozoic granitoid rocks in the Jiaobei Terrane,North China Craton.Precambrian Research,255:685-698
Liu XY.2011.Chronological,petrological and geochemical characteristics of the paleo-Mesoproterozoic alkali-rich intrusive rocks along the southern part of the North China Craton.Master Degree Thesis.Beijing:Chinese Academy of Geological Sciences(in Chinese with English summary)
Liu Y,Liu HC and Li XH.1996.Simultaneous and precise determination of 40 trace elements in rock samples using ICP-MS.Geochimica,25(6):552-558(in Chinese with English abstract)
Loiselle MC and Wones DR.1979.Characteristics and origin of anorogenic granites.Geological of Society of America,11(7):468
Lu SN,Li HK,Li HM,Song B,Wang SY,Zhou HY and Chen ZH.2003.U-Pb isotopic ages and their significance of alkaline granite in the southern margin of the North China Craton.Geological Bulletin of China,22(10):762-768(in Chinese with English abstract)
Lu SN,Zhao GC,Wang HC and Hao GJ.2008.Precambrian metamorphic basement and sedimentary cover of the North China Craton:A review.Precambrian Research,160(1-2):77-93
Ma GX,Liu FY,Su L,Han YG and Wang QH.2013.LA-ICP-MSzircon U-Pb age from the Proterozoic syenite in Xiaoqinling area in the North China Craton and its geological implications.Journal of Jilin University(Earth Science Edition),43(5):1457-1470(in Chinese with English abstract)
Pati1o Douce AE.1997.Generation of metaluminous A-type granites by low-pressure melting of calc-alkaline granitoids.Geology,25(8):743-746
Pearce JA,Harris NBW and Tindle AG.1984.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks.Journal of Petrology,25(4):956-983
Pearce JA.1996.Sources and settings of granitic rocks.Episodes,19(4):120-125
Peng P,Zhai MG,Zhang HF,Zhao TP and Ni ZY.2004.Geochemistry and geological significance of the 1.8Ga mafic dyke swarms in the North China Craton:An example from the juncture of Shanxi,Hebei and Inner Mongolia.Acta Petrologica Sinica,20(3):439-456(in Chinese with English abstract)
Peng P,Zhai MG,Ernst RE,Guo JH,Liu F and Hu B.2008.A1.78Ga large igneous province in the North China craton:The Xiong’er volcanic province and the North China dyke swarm.Lithos,101(3-4):260-280
Peng P,Liu F,Zhai MG and Guo JH.2012.Age of the Miyun dyke swarm:Constraints on the maximum depositional age of the Changcheng System.Chinese Science Bulletin,57(1):105-110
Peng P.2015.Precambrian mafic dyke swarms in the North China Craton and their geological implications.Science China(Earth Sciences),58(5):649-675
Rm9 OT,Haapala I,Vaasjoki M,Yu JH and Fu HQ.1995.1700Ma Shachang complex,northeast China:Proterozoic rapakivi granite not associated with Paleoproterozoic orogenic crust.Geology,23(9):815-818
Ren FG,Li HM,Yin YJ,Li SB,Ding SY and Chen ZH.2000.The upper chronological limit of Xionger Group’s volcanic rock series,and its geological significance.Progress in Precambrian Research,23(3):140-146(in Chinese with English abstract)
Ren KX,Yan GH,Cai JH,Mu BL,Li FT,Wang YB and Chu ZY.2006.Chronology and geological implication of the Paleo-Mesoproterozoic alkaline-rich intrusions belt from the northern part in the North China Craton.Acta Petrologica Sinica,22(2):377-386(in Chinese with English abstract)
Shellnutt JG,Wang CY,Zhou MF and Yang YH.2009.Zircon Lu-Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province(SW China):Constraints on the mantle source.Journal of Asian Earth Sciences,35(1):45-55
Shi JP,Yang DB,Huo TF,Yang HT,Xu WL and Wang F.2017.The geochronology and Nd-Hf isotope compositions of A-type granites on the southern margin of North China Craton:Constraints on the Late Paleoproterozoic extensional events.Acta Petrologica Sinica,33(10):3042-3056(in Chinese with English abstract)
Sun SS and McD onough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Valley JW,Kinny PD,Schulze DJ and Spicuzza MJ.1998.Zircon megacrysts from kimberlite:Oxygen isotope variability among mantle melts.Contributions to Mineralogy and Petrology,133(1-2):1-11
Wan YS,Liu DY,Wang SY,Zhao X,Dong CY,Zhou HY,Yin XY,Yang CX and Gao LZ.2009.Early Precambrian crustal evolution in the Dengfeng area,Henan Province(eastern China):Constraints from geochemistry and SHRIMP U-Pb zircon dating.Acta Geologica Sinica,83(7):982-999(in Chinese with English abstract)
Wang J,Wu YB,Gao S,Peng M,Liu XC,Zhao LS,Zhou L,Hu ZC,Gong HJ and Liu YS.2010.Zircon U-Pb and trace element data from rocks of the Huai’an Complex:New insights into the late Paleoproterozoic collision between the Eastern and Western blocks of the North China Craton.Precambrian Research,178(1-4):59-71
Wang XL,Jiang SY,Dai BZ and Kern J.2013.Lithospheric thinning and reworking of Late Archean juvenile crust on the southern margin of the North China Craton:Evidence from the Longwangzhuang Paleoproterozoic A-type granites and their surrounding Cretaceous adakite-like granites.Geological Journal,48(5):498-515
Wang YJ,Fan WM,Zhang YH,Guo F,Zhang HF and Peng TP.2004.Geochemical,40Ar/39Ar geochronological and Sr-Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca.1800Ma event of the North China Craton.Precambrian Research,135(1-2):55-77
Wang YJ,Zhao GC,Fan WM,Peng TP,Sun LH and Xia XP.2007.LA-ICP-MS U-Pb zircon geochronology and geochemistry of Paleoproterozoic mafic dykes from western Shandong Province:Implications for back-arc basin magmatism in the Eastern Block,North China Craton.Precambrian Research,154(1-2):107-124
Wang YJ,Zhao GC,Cawood PA,Fan WM,Peng TP and Sun LH.2008.Geochemistry of Paleoproterozoic(~1770Ma)mafic dikes from the Trans-North China Orogen and tectonic implications.Journal of Asian Earth Sciences,33(1-2):61-77
Whalen JB,Currie KL and Chappell BW.1987.A-type granites:Geochemical characteristics,discrimination and petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419
Wilson M.1989.Igneous Petrogenesis:A Global Tectonic Approach.London:Chapman&Hall,13-34
Wu FY,Sun DY,Li HM,Jahn BM and Wilde S.2002.A-type granites in northeastern China:Age and geochemical constraints on their petrogenesis.Chemical Geology,187(1-2):143-173
Wu FY,Li XH,Yang JH and Zheng YF.2007.Discussions on the petrogenesis of granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract)
Yan J,Peng G,Liu JM,Li QZ,Chen ZH,Shi L,Liu XQ and Jiang ZZ.2012.Petrogenesis of granites from Fanchang district,the Lower Yangtze region:Zircon geochronology and Hf-O isotopes constrains.Acta Petrologica Sinica,28(10):3209-3227(in Chinese withEnglish abstract)
Yang JH,Wu FY,Chung SL,Wilde SA and Chu MF.2006.A hybrid origin for the Qianshan A-type granite,northeast China:Geochemical and Sr-Nd-Hf isotopic evidence.Lithos,89(1-2):89-106
Zhai MG,Santosh M and Zhang LC.2011.Precambrian geology and tectonic evolution of the North China Craton.Gondwana Research,20(1):1-5
Zhai MG,Hu B,Peng P and Zhao TP.2014.Meso-Neoproterozoic magmatic events and multi-stage rifting in the NCC.Earth Science Frontiers,21(1):100-119(in Chinese with English abstract)
Zhang J,Zhang HF and Lu XX.2013.Zircon U-Pb age and Lu-Hf isotope constraints on Precambrian evolution of continental crust in the Songshan area,the south-central North China Craton.Precambrian Research,226:1-20
Zhao GC,Wilde SA,Sun M,Li SZ,Li XP and Zhang J.2008a.SHRIMP U-Pb zircon ages of granitoid rocks in the Lüliang Complex:Implications for the accretion and evolution of the Trans-North China Orogen.Precambrian Research,160(3-4):213-226
Zhao GC,He YH and Sun M.2009.The Xiong’er volcanic belt at the southern margin of the North China Craton:Petrographic and geochemical evidence for its outboard position in the PaleoMesoproterozoic Columbia supercontinent.Gondwana Research,16(2):170-181
Zhao GC and Cawood PA.2012.Precambrian geology of China.Precambrian Research,222-223:13-54
Zhao GC,Cawood PA,Li SZ,Wilde SA,Sun M,Zhang J,He YH and Yin CQ.2012.Amalgamation of the North China Craton:Key issues and discussion.Precambrian Research,222-223:55-76
Zhao J,Zhang CL,Guo XJ and Liu XY.2018.The late-Paleoproterozoic I-and A-type granites in Lüliang complex,North China craton:New evidence on post-collisional extension of Trans-North China Orogen.Precambrian Research,318:70-88
Zhao TP,Zhou MF,Zhai MG and Xia B.2002.Paleoproterozoic riftrelated volcanism of the Xiong’er group,North China craton:Implications for the breakup of Columbia.International Geology Review,44(4):336-351
Zhao TP,Chen FK,Zhai MG and Xia B.2004.Single zircon U-Pb ages and their geological significance of the Damiao anorthosite complex,Hebei Province,China.Acta Petrologica Sinica,20(3):685-690(in Chinese with English abstract)
Zhao TP and Zhou MF.2009.Geochemical constraints on the tectonic setting of Paleoproterozoic A-type granites in the southern margin of the North China Craton.Journal of Asian Earth Sciences,36(2-3):183-195
Zhao TP,Deng XQ,Hu GH,Zhou YY,Peng P and Zhai MG.2015.The Paleoproterozoic-Mesoproterozoic boundary of the North China Craton and the related geological issues:A review.Acta Petrologica Sinica,31(6):1495-1508(in Chinese with English abstract)
Zhao XF,Zhou MF,Li JW and Wu FY.2008b.Association of Neoproterozoic A-and I-type granites in South China:Implications for generation of A-type granites in a subduction-related environment.Chemical Geology,257(1-2):1-15
Zhao ZP.1993.Precambrian Crustal Evolution of the Sino-Korean Paraplatform.Beijing:Science Press(in Chinese)
Zhou YY,Zhai MG,Zhao TP,Lan ZW and Sun QY.2014.Geochronological and geochemical constraints on the petrogenesis of the Early Paleoproterozoic potassic granite in the Lushan area,southern margin of the North China Craton.Journal of Asian Earth Sciences,94:190-204
白瑾,黄学光,王慧初等.1996.中国前寒武纪地壳演化.北京:地质出版社
包志伟,王强,资锋,唐功建,杜凤军,白国典.2009.龙王A型花岗岩地球化学特征及其地球动力学意义.地球化学,38(6):509-522
邓小芹,赵太平,彭头平,高昕宇,包志伟.2015.华北克拉通南缘1600Ma麻坪A型花岗岩的成因及其地质意义.岩石学报,31(6):1621-1635
第五春荣,孙勇,林慈銮,王洪亮.2010.河南鲁山地区太华杂岩LA-(MC)-ICPMS锆石U-Pb年代学及Hf同位素组成.科学通报,55(21):2112-2123
高山林,林晋炎,陆彦俊.2013.宁夏泾源石咀子古元古代A型花岗岩的形成时代及其地质意义.岩石学报,29(8):2676-2684
耿元生,杨崇辉,万渝生.2006.吕梁地区古元古代花岗岩浆作用---来自同位素年代学的证据.岩石学报,22(2):305-314
郭波,朱赖民,李犇,弓虎军,王建其.2009.华北陆块南缘华山和合峪花岗岩岩体锆石U-Pb年龄、Hf同位素组成与成岩动力学背景.岩石学报,25(2):265-281
郭敬辉,石昕,卞爱国,许荣华,翟明国,李永刚.1999.桑干地区早元古代花岗岩长石Pb同位素组成和锆石U-Pb年龄:变质与地壳熔融作用及构造-热事件演化.岩石学报,15(2):199-207
胡国辉,胡俊良,陈伟,赵太平.2010.华北克拉通南缘中条山-嵩山地区1.78Ga基性岩墙群的地球化学特征及构造环境.岩石学报,26(5):1563-1576
柳晓艳.2011.华北克拉通南缘古-中元古代碱性岩岩石地球化学与年代学研究及其地质意义.硕士学位论文.北京:中国地质科学院
刘颖,刘海臣,李献华.1996.用ICP-MS准确测定岩石样品中的40余种微量元素.地球化学,25(6):552-558
陆松年,李怀坤,李惠民,宋彪,王世炎,周红英,陈志宏.2003.华北克拉通南缘龙王碱性花岗岩U-Pb年龄及其地质意义.地质通报,22(10):762-768
马桂霞,刘富营,苏犁,韩衣贵,王清海.2013.华北克拉通小秦岭地区元古宙正长岩LA-ICP-MS锆石U-Pb年龄及其地质意义.吉林大学学报(地球科学版),43(5):1457-1470
彭澎,翟明国,张华锋,赵太平,倪志耀.2004.华北克拉通1.8Ga镁铁质岩墙群的地球化学特征及其地质意义:以晋冀蒙交界地区为例.岩石学报,20(3):439-456
彭澎,刘富,翟明国,郭敬辉.2011.密云岩墙群的时代及其对长城系底界年龄的制约.科学通报,56(35):2975-2980
全国地层委员会.2002.中国区域年代地层(地质年代)表说明书.北京:地质出版社
任富根,李惠民,殷艳杰,李双保,丁士应,陈志宏.2000.熊耳群火山岩系的上限年龄及其地质意义.前寒武纪研究进展,23(3):140-146
任康绪,阎国翰,蔡剑辉,牟保磊,李凤棠,王彦斌,储著银.2006.华北克拉通北部地区古-中元古代富碱侵入岩年代学及意义.岩石学报,22(2):377-386
陕西省地质矿产局.1989.陕西省区域地质志.北京:地质出版社
师江朋,杨德彬,霍腾飞,杨浩田,许文良,王枫.2017.华北克拉通南缘A型花岗岩的年代学和Nd-Hf同位素组成:对古元古代晚期伸展事件的制约.岩石学报,33(10):3042-3056
万渝生,刘敦一,王世炎,赵逊,董春艳,周红英,殷小艳,杨长秀,高林志.2009.登封地区早前寒武纪地壳演化-地球化学和锆石SHRIMP U-Pb年代学制约.地质学报,83(7):982-999
吴福元,李献华,杨进辉,郑永飞.2007.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238
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
翟明国,胡波,彭澎,赵太平.2014.华北中-新元古代的岩浆作用与多期裂谷事件.地学前缘,21(1):100-119
赵太平,陈福坤,翟明国,夏斌.2004.河北大庙斜长岩杂岩体锆石U-Pb年龄及其地质意义.岩石学报,20(3):685-690
赵太平,邓小芹,胡国辉,周艳艳,彭澎,翟明国.2015.华北克拉通古/中元古代界线和相关地质问题讨论.岩石学报,31(6):1495-1508
赵宗溥.1993.中朝准地台前寒武纪地壳演化.北京:科学出版社
Anderson JL and Bender EE.1989.Nature and origin of Proterozoic A-type granitic magmatism in the southwestern United States of America.Lithos,23(1-2):19-52
Bai J,Huang XG,Wang HC et al.1996.The Precambrian Crustal Evolution of China.Beijing:Geological Publishing House(in Chinese)
Bao ZW,Wang Q,Zi F,Tang GJ,Du FJ and Bai GD.2009.Geochemistry of the Paleoproterozoic Longwangzhuang A-type granites on the southern margin of North China Craton:Petrogenesis and tectonic implications.Geochimica,38(6):509-522(in Chinese with English abstract)
Belousova EA,Griffin WL,O’Reilly SY and Fisher NI.2002.Igneous zircon:Trace element composition as an indicator of source rock type.Contributions to Mineralogy and Petrology,143(5):602-622
Bindeman I.2008.Oxygen isotopes in mantle and crustal magmas as revealed by single crystal analysis.Reviews in Mineralogy and Geochemistry,69(1):445-478
Bonin B.2007.A-type granites and related rocks:Evolution of a concept,problems and prospects.Lithos,97(1-2):1-29
Bureau of Geology and Mineral Resources of Shaanxi Province(BGMRS).1989.Regional Geology of Shaanxi Province.Beijing:Geological Publishing House(in Chinese)
Collins WJ,Beams SD,White AJR and Chappell BW.1982.Nature and origin of A-type granites with particular reference to southeastern Australia.Contributions to Mineralogy and Petrology,80(2):189-200
Creaser RA,Price RC and Wormald RJ.1991.A-type granites revisited:Assessment of a residual-source model.Geology,19(2):163-166
Dall’Agnol R,Frost CD and Rm9 OT.2012.IGCP Project 510“A-type granites and related rocks through time”:Project vita,results,and contribution to granite research.Lithos,151:1-16
Deng XQ,Zhao TP,Peng TP,Gao XY and Bao ZW.2015.Petrogenesis of 1600Ma Maping A-type granite in the southern margin of the North China Craton and its tectonic implications.Acta Petrologica Sinica,31(6):1621-1635(in Chinese with English abstract)
Deng XQ,Zhao TP and Peng TP.2016a.Age and geochemistry of the Early Mesoproterozoic A-type granites in the southern margin of the North China Craton:Constraints on their petrogenesis and tectonic implications.Precambrian Research,283:68-88
Deng XQ,Peng TP and Zhao TP.2016b.Geochronology and geochemistry of the late Paleoproterozoic aluminous A-type granite in the Xiaoqinling area along the southern margin of the North China Craton:Petrogenesis and tectonic implications.Precambrian Research,285:127-146
Diwu CR,Sun Y,Lin CL and Wang HL.2010.LA-(MC)-ICPMS U-Pb zircon geochronology and Lu-Hf isotope compositions of the Taihua Complex on the southern margin of the North China Craton.Chinese Science Bulletin,55(23):2557-2571
Diwu CR,Sun Y,Zhao Y and Lai SC.2014.Early Paleoproterozoic(2.45~2.20Ga)magmatic activity during the period of global magmatic shutdown:Implications for the crustal evolution of the southern North China Craton.Precambrian Research,255:627-640
Eby GN.1990.The A-type granitoids:A review of their occurrence and chemical characteristics and speculations on their petrogenesis.Lithos,26(1-2):115-134
Eby GN.1992.Chemical subdivision of the A-type granitoids:Petrogenetic and tectonic implications.Geology,20(7):641-644
Frost CD,Rm9 OT and Dall’Agnol R.2007.IGCP project 510-A-type granites and related rocks through time.Lithos,97(1-2):Vii-Xiii
Frost CD and Frost BR.2011.On ferroan(A-type)granitoids:Their compositional variability and modes of origin.Journal of Petrology,52(1):39-53
Gao SL,Lin JY and Lu YJ.2013.Formation epoch and its geological implications of Paleoprotozoic A-type granite in Shizuizi of Jingyuan County,Ningxia Province.Acta Petrologica Sinica,29(8):2676-2684(in Chinese with English abstract)
Geng YS,Yang CH and Wan YS.2006.Paleoproterozoic granitic magmatism in the Luliang area,North China Craton:Constraint from isotopic geochronology.Acta Petrologica Sinica,22(2):305-314(in Chinese with English abstract)
Guo B,Zhu LM,Li B,Gong HJ and Wang JQ.2009.Zircon U-Pb age and Hf isotope composition of the Huashan and Heyu granite plutons at the southern margin of North China Craton:Implications for geodynamic setting.Acta Petrologica Sinica,25(2):265-281(in Chinese with English abstract)
Guo JH,Shi X,Bian AG,Xu RH,Zhai MG and Li YG.1999.Pb isotopic composition of feldspar and U-Pb age of zircon from early Proterozoic granite in Sanggan area,North China craton:Metamorphism,crustal melting and tectono-thermal event.Acta Petrologica Sinica,15(2):199-207(in Chinese with English abstract)
Hou GT,Liu YL and Li JH.2006.Evidence for~1.8Ga extension of the eastern Block of the North China Craton from SHRIMP U-Pb dating of mafic dyke swarms in Shandong Province.Journal of Asian Earth Sciences,27(4):392-401
Hu GH,Hu JL,Chen W and Zhao TP.2010.Geochemistry and tectonic setting of the 1.78Ga mafic dyke swarms in the Mt.Zhongtiao and Mt.Song areas,the southern margin of the North China Craton.Acta Petrologica Sinica,26(5):1563-1576(in Chinese with English abstract)
Huang HQ,Li XH,Li WX and Li ZX.2011.Formation of highδ18Ofayalite-bearing A-type granite by high-temperature melting of granulitic metasedimentary rocks,southern China.Geology,39(10):903-906
King PL,White AJR,Chappell BW and Allen CM.1997.Characterization and origin of aluminous A-type granites from the Lachlan Fold Belt,southeastern Australia.Journal of Petrology,38(3):371-391
Li XH,Liu Y,Li QL,Guo CH and Chamberlain KR.2009.Precise determination of Phanerozoic zircon Pb/Pb age by multicollector SIMS without external standardization.Geochemistry,Geophysics,Geosystems,10(4):Q04010
Liu JH,Liu FL,Ding ZJ,Liu PH,Guo CL and Wang F.2014.Geochronology,petrogenesis and tectonic implications of Paleoproterozoic granitoid rocks in the Jiaobei Terrane,North China Craton.Precambrian Research,255:685-698
Liu XY.2011.Chronological,petrological and geochemical characteristics of the paleo-Mesoproterozoic alkali-rich intrusive rocks along the southern part of the North China Craton.Master Degree Thesis.Beijing:Chinese Academy of Geological Sciences(in Chinese with English summary)
Liu Y,Liu HC and Li XH.1996.Simultaneous and precise determination of 40 trace elements in rock samples using ICP-MS.Geochimica,25(6):552-558(in Chinese with English abstract)
Loiselle MC and Wones DR.1979.Characteristics and origin of anorogenic granites.Geological of Society of America,11(7):468
Lu SN,Li HK,Li HM,Song B,Wang SY,Zhou HY and Chen ZH.2003.U-Pb isotopic ages and their significance of alkaline granite in the southern margin of the North China Craton.Geological Bulletin of China,22(10):762-768(in Chinese with English abstract)
Lu SN,Zhao GC,Wang HC and Hao GJ.2008.Precambrian metamorphic basement and sedimentary cover of the North China Craton:A review.Precambrian Research,160(1-2):77-93
Ma GX,Liu FY,Su L,Han YG and Wang QH.2013.LA-ICP-MSzircon U-Pb age from the Proterozoic syenite in Xiaoqinling area in the North China Craton and its geological implications.Journal of Jilin University(Earth Science Edition),43(5):1457-1470(in Chinese with English abstract)
Pati1o Douce AE.1997.Generation of metaluminous A-type granites by low-pressure melting of calc-alkaline granitoids.Geology,25(8):743-746
Pearce JA,Harris NBW and Tindle AG.1984.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks.Journal of Petrology,25(4):956-983
Pearce JA.1996.Sources and settings of granitic rocks.Episodes,19(4):120-125
Peng P,Zhai MG,Zhang HF,Zhao TP and Ni ZY.2004.Geochemistry and geological significance of the 1.8Ga mafic dyke swarms in the North China Craton:An example from the juncture of Shanxi,Hebei and Inner Mongolia.Acta Petrologica Sinica,20(3):439-456(in Chinese with English abstract)
Peng P,Zhai MG,Ernst RE,Guo JH,Liu F and Hu B.2008.A1.78Ga large igneous province in the North China craton:The Xiong’er volcanic province and the North China dyke swarm.Lithos,101(3-4):260-280
Peng P,Liu F,Zhai MG and Guo JH.2012.Age of the Miyun dyke swarm:Constraints on the maximum depositional age of the Changcheng System.Chinese Science Bulletin,57(1):105-110
Peng P.2015.Precambrian mafic dyke swarms in the North China Craton and their geological implications.Science China(Earth Sciences),58(5):649-675
Rm9 OT,Haapala I,Vaasjoki M,Yu JH and Fu HQ.1995.1700Ma Shachang complex,northeast China:Proterozoic rapakivi granite not associated with Paleoproterozoic orogenic crust.Geology,23(9):815-818
Ren FG,Li HM,Yin YJ,Li SB,Ding SY and Chen ZH.2000.The upper chronological limit of Xionger Group’s volcanic rock series,and its geological significance.Progress in Precambrian Research,23(3):140-146(in Chinese with English abstract)
Ren KX,Yan GH,Cai JH,Mu BL,Li FT,Wang YB and Chu ZY.2006.Chronology and geological implication of the Paleo-Mesoproterozoic alkaline-rich intrusions belt from the northern part in the North China Craton.Acta Petrologica Sinica,22(2):377-386(in Chinese with English abstract)
Shellnutt JG,Wang CY,Zhou MF and Yang YH.2009.Zircon Lu-Hf isotopic compositions of metaluminous and peralkaline A-type granitic plutons of the Emeishan large igneous province(SW China):Constraints on the mantle source.Journal of Asian Earth Sciences,35(1):45-55
Shi JP,Yang DB,Huo TF,Yang HT,Xu WL and Wang F.2017.The geochronology and Nd-Hf isotope compositions of A-type granites on the southern margin of North China Craton:Constraints on the Late Paleoproterozoic extensional events.Acta Petrologica Sinica,33(10):3042-3056(in Chinese with English abstract)
Sun SS and McD onough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in the Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Valley JW,Kinny PD,Schulze DJ and Spicuzza MJ.1998.Zircon megacrysts from kimberlite:Oxygen isotope variability among mantle melts.Contributions to Mineralogy and Petrology,133(1-2):1-11
Wan YS,Liu DY,Wang SY,Zhao X,Dong CY,Zhou HY,Yin XY,Yang CX and Gao LZ.2009.Early Precambrian crustal evolution in the Dengfeng area,Henan Province(eastern China):Constraints from geochemistry and SHRIMP U-Pb zircon dating.Acta Geologica Sinica,83(7):982-999(in Chinese with English abstract)
Wang J,Wu YB,Gao S,Peng M,Liu XC,Zhao LS,Zhou L,Hu ZC,Gong HJ and Liu YS.2010.Zircon U-Pb and trace element data from rocks of the Huai’an Complex:New insights into the late Paleoproterozoic collision between the Eastern and Western blocks of the North China Craton.Precambrian Research,178(1-4):59-71
Wang XL,Jiang SY,Dai BZ and Kern J.2013.Lithospheric thinning and reworking of Late Archean juvenile crust on the southern margin of the North China Craton:Evidence from the Longwangzhuang Paleoproterozoic A-type granites and their surrounding Cretaceous adakite-like granites.Geological Journal,48(5):498-515
Wang YJ,Fan WM,Zhang YH,Guo F,Zhang HF and Peng TP.2004.Geochemical,40Ar/39Ar geochronological and Sr-Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca.1800Ma event of the North China Craton.Precambrian Research,135(1-2):55-77
Wang YJ,Zhao GC,Fan WM,Peng TP,Sun LH and Xia XP.2007.LA-ICP-MS U-Pb zircon geochronology and geochemistry of Paleoproterozoic mafic dykes from western Shandong Province:Implications for back-arc basin magmatism in the Eastern Block,North China Craton.Precambrian Research,154(1-2):107-124
Wang YJ,Zhao GC,Cawood PA,Fan WM,Peng TP and Sun LH.2008.Geochemistry of Paleoproterozoic(~1770Ma)mafic dikes from the Trans-North China Orogen and tectonic implications.Journal of Asian Earth Sciences,33(1-2):61-77
Whalen JB,Currie KL and Chappell BW.1987.A-type granites:Geochemical characteristics,discrimination and petrogenesis.Contributions to Mineralogy and Petrology,95(4):407-419
Wilson M.1989.Igneous Petrogenesis:A Global Tectonic Approach.London:Chapman&Hall,13-34
Wu FY,Sun DY,Li HM,Jahn BM and Wilde S.2002.A-type granites in northeastern China:Age and geochemical constraints on their petrogenesis.Chemical Geology,187(1-2):143-173
Wu FY,Li XH,Yang JH and Zheng YF.2007.Discussions on the petrogenesis of granites.Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract)
Yan J,Peng G,Liu JM,Li QZ,Chen ZH,Shi L,Liu XQ and Jiang ZZ.2012.Petrogenesis of granites from Fanchang district,the Lower Yangtze region:Zircon geochronology and Hf-O isotopes constrains.Acta Petrologica Sinica,28(10):3209-3227(in Chinese withEnglish abstract)
Yang JH,Wu FY,Chung SL,Wilde SA and Chu MF.2006.A hybrid origin for the Qianshan A-type granite,northeast China:Geochemical and Sr-Nd-Hf isotopic evidence.Lithos,89(1-2):89-106
Zhai MG,Santosh M and Zhang LC.2011.Precambrian geology and tectonic evolution of the North China Craton.Gondwana Research,20(1):1-5
Zhai MG,Hu B,Peng P and Zhao TP.2014.Meso-Neoproterozoic magmatic events and multi-stage rifting in the NCC.Earth Science Frontiers,21(1):100-119(in Chinese with English abstract)
Zhang J,Zhang HF and Lu XX.2013.Zircon U-Pb age and Lu-Hf isotope constraints on Precambrian evolution of continental crust in the Songshan area,the south-central North China Craton.Precambrian Research,226:1-20
Zhao GC,Wilde SA,Sun M,Li SZ,Li XP and Zhang J.2008a.SHRIMP U-Pb zircon ages of granitoid rocks in the Lüliang Complex:Implications for the accretion and evolution of the Trans-North China Orogen.Precambrian Research,160(3-4):213-226
Zhao GC,He YH and Sun M.2009.The Xiong’er volcanic belt at the southern margin of the North China Craton:Petrographic and geochemical evidence for its outboard position in the PaleoMesoproterozoic Columbia supercontinent.Gondwana Research,16(2):170-181
Zhao GC and Cawood PA.2012.Precambrian geology of China.Precambrian Research,222-223:13-54
Zhao GC,Cawood PA,Li SZ,Wilde SA,Sun M,Zhang J,He YH and Yin CQ.2012.Amalgamation of the North China Craton:Key issues and discussion.Precambrian Research,222-223:55-76
Zhao J,Zhang CL,Guo XJ and Liu XY.2018.The late-Paleoproterozoic I-and A-type granites in Lüliang complex,North China craton:New evidence on post-collisional extension of Trans-North China Orogen.Precambrian Research,318:70-88
Zhao TP,Zhou MF,Zhai MG and Xia B.2002.Paleoproterozoic riftrelated volcanism of the Xiong’er group,North China craton:Implications for the breakup of Columbia.International Geology Review,44(4):336-351
Zhao TP,Chen FK,Zhai MG and Xia B.2004.Single zircon U-Pb ages and their geological significance of the Damiao anorthosite complex,Hebei Province,China.Acta Petrologica Sinica,20(3):685-690(in Chinese with English abstract)
Zhao TP and Zhou MF.2009.Geochemical constraints on the tectonic setting of Paleoproterozoic A-type granites in the southern margin of the North China Craton.Journal of Asian Earth Sciences,36(2-3):183-195
Zhao TP,Deng XQ,Hu GH,Zhou YY,Peng P and Zhai MG.2015.The Paleoproterozoic-Mesoproterozoic boundary of the North China Craton and the related geological issues:A review.Acta Petrologica Sinica,31(6):1495-1508(in Chinese with English abstract)
Zhao XF,Zhou MF,Li JW and Wu FY.2008b.Association of Neoproterozoic A-and I-type granites in South China:Implications for generation of A-type granites in a subduction-related environment.Chemical Geology,257(1-2):1-15
Zhao ZP.1993.Precambrian Crustal Evolution of the Sino-Korean Paraplatform.Beijing:Science Press(in Chinese)
Zhou YY,Zhai MG,Zhao TP,Lan ZW and Sun QY.2014.Geochronological and geochemical constraints on the petrogenesis of the Early Paleoproterozoic potassic granite in the Lushan area,southern margin of the North China Craton.Journal of Asian Earth Sciences,94:190-204
白瑾,黄学光,王慧初等.1996.中国前寒武纪地壳演化.北京:地质出版社
包志伟,王强,资锋,唐功建,杜凤军,白国典.2009.龙王A型花岗岩地球化学特征及其地球动力学意义.地球化学,38(6):509-522
邓小芹,赵太平,彭头平,高昕宇,包志伟.2015.华北克拉通南缘1600Ma麻坪A型花岗岩的成因及其地质意义.岩石学报,31(6):1621-1635
第五春荣,孙勇,林慈銮,王洪亮.2010.河南鲁山地区太华杂岩LA-(MC)-ICPMS锆石U-Pb年代学及Hf同位素组成.科学通报,55(21):2112-2123
高山林,林晋炎,陆彦俊.2013.宁夏泾源石咀子古元古代A型花岗岩的形成时代及其地质意义.岩石学报,29(8):2676-2684
耿元生,杨崇辉,万渝生.2006.吕梁地区古元古代花岗岩浆作用---来自同位素年代学的证据.岩石学报,22(2):305-314
郭波,朱赖民,李犇,弓虎军,王建其.2009.华北陆块南缘华山和合峪花岗岩岩体锆石U-Pb年龄、Hf同位素组成与成岩动力学背景.岩石学报,25(2):265-281
郭敬辉,石昕,卞爱国,许荣华,翟明国,李永刚.1999.桑干地区早元古代花岗岩长石Pb同位素组成和锆石U-Pb年龄:变质与地壳熔融作用及构造-热事件演化.岩石学报,15(2):199-207
胡国辉,胡俊良,陈伟,赵太平.2010.华北克拉通南缘中条山-嵩山地区1.78Ga基性岩墙群的地球化学特征及构造环境.岩石学报,26(5):1563-1576
柳晓艳.2011.华北克拉通南缘古-中元古代碱性岩岩石地球化学与年代学研究及其地质意义.硕士学位论文.北京:中国地质科学院
刘颖,刘海臣,李献华.1996.用ICP-MS准确测定岩石样品中的40余种微量元素.地球化学,25(6):552-558
陆松年,李怀坤,李惠民,宋彪,王世炎,周红英,陈志宏.2003.华北克拉通南缘龙王碱性花岗岩U-Pb年龄及其地质意义.地质通报,22(10):762-768
马桂霞,刘富营,苏犁,韩衣贵,王清海.2013.华北克拉通小秦岭地区元古宙正长岩LA-ICP-MS锆石U-Pb年龄及其地质意义.吉林大学学报(地球科学版),43(5):1457-1470
彭澎,翟明国,张华锋,赵太平,倪志耀.2004.华北克拉通1.8Ga镁铁质岩墙群的地球化学特征及其地质意义:以晋冀蒙交界地区为例.岩石学报,20(3):439-456
彭澎,刘富,翟明国,郭敬辉.2011.密云岩墙群的时代及其对长城系底界年龄的制约.科学通报,56(35):2975-2980
全国地层委员会.2002.中国区域年代地层(地质年代)表说明书.北京:地质出版社
任富根,李惠民,殷艳杰,李双保,丁士应,陈志宏.2000.熊耳群火山岩系的上限年龄及其地质意义.前寒武纪研究进展,23(3):140-146
任康绪,阎国翰,蔡剑辉,牟保磊,李凤棠,王彦斌,储著银.2006.华北克拉通北部地区古-中元古代富碱侵入岩年代学及意义.岩石学报,22(2):377-386
陕西省地质矿产局.1989.陕西省区域地质志.北京:地质出版社
师江朋,杨德彬,霍腾飞,杨浩田,许文良,王枫.2017.华北克拉通南缘A型花岗岩的年代学和Nd-Hf同位素组成:对古元古代晚期伸展事件的制约.岩石学报,33(10):3042-3056
万渝生,刘敦一,王世炎,赵逊,董春艳,周红英,殷小艳,杨长秀,高林志.2009.登封地区早前寒武纪地壳演化-地球化学和锆石SHRIMP U-Pb年代学制约.地质学报,83(7):982-999
吴福元,李献华,杨进辉,郑永飞.2007.花岗岩成因研究的若干问题.岩石学报,23(6):1217-1238
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
翟明国,胡波,彭澎,赵太平.2014.华北中-新元古代的岩浆作用与多期裂谷事件.地学前缘,21(1):100-119
赵太平,陈福坤,翟明国,夏斌.2004.河北大庙斜长岩杂岩体锆石U-Pb年龄及其地质意义.岩石学报,20(3):685-690
赵太平,邓小芹,胡国辉,周艳艳,彭澎,翟明国.2015.华北克拉通古/中元古代界线和相关地质问题讨论.岩石学报,31(6):1495-1508
赵宗溥.1993.中朝准地台前寒武纪地壳演化.北京:科学出版社
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |