中生代华北克拉通岩石圈减薄的证据——以河北武安固镇杂岩体为例
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摘要
本文对位于华北克拉通中部的固镇侵入杂岩体(闪长岩、二长岩、石英二长岩和正长岩)进行了野外地质调查、岩相学、矿物学、地球化学、锆石U-Pb定年、Sr-Nd同位素和Lu-Hf同位素研究,进而探讨其形成时代、源区和成因,以期得到关于华北克拉通中部中生代岩石圈减薄研究的新启示。研究区岩体形成时代和岩石结构有一定关联性,总体来看,等粒结构的岩体形成时代早于似斑状结构岩体,研究区岩浆活动可分为两个期次:第一期次岩浆活动形成等粒结构的深成岩体,包括中细粒闪长岩、二长岩、石英二长岩和正长岩,形成时代约为130～135Ma;第二期次岩浆活动形成浅部的似斑状岩体,包括似斑状闪长岩和石英二长岩,形成时代约为127Ma。结合野外观察、岩相学、矿物学、地球化学等特征,讨论分析了固镇杂岩体的成因:固镇闪长岩富镁,高Mg~#值,Cr、Ni含量较高,富集LILE和LREE,亏损HFSE,铕异常不明显,具有高镁安山岩(HMA)性质,是与其相对应的侵入岩。固镇高镁闪长岩是被俯冲板片熔体和流体交代后的地幔橄榄岩部分熔融的产物,岩浆在上升途中与地壳发生了较弱的同化混染。固镇正长岩形成于加厚陆壳的部分熔融,地壳厚度约为40～67km。固镇二长岩是由区内正长岩和高镁闪长岩混合形成。研究区石英二长岩是区内高镁闪长岩与另一种更富硅的岩浆混合形成。俯冲板片物质(流体+熔体)对固镇高镁闪长岩的形成有重要贡献,显示出古太平洋板块俯冲作用的影响也涉及到了NCC中部,但受影响的程度小于NCC东部;正长岩形成于加厚陆壳部分熔融,显示出拆沉作用在中生代NCC中部岩石圈减薄过程中发挥了重要作用。结合角闪石温压计的计算结果和前人研究成果可以推测,NCC中部大规模拆沉作用发生的时间节点为127Ma。
This paper takes the Guzhen intrusive complex which is located in Hebei Province in the central part of the North China Craton( NCC) as a research object. The author conducted detailed field geological survey,combined with indoor research,including petrography,mineralogy,geochemistry,Sr-Nd isotope,Lu-Hf isotope and U-Pb zircon chronology analysis,so as to explore the formation age,source area,petrogenesis of Guzhen intrusive complex,in order to draw new inspiration for the Mesozoic lithospheric thinning in the central NCC. In this paper,it is believed that the formation age of the Guzhen complex is related to the structure of the rock. The formation age of the rock with equal grain structure is earlier than that of the rock with porphyritic structure. Magmatic activity can be divided into two phases: the first stage( 130 ～ 135 Ma) magmatic activity forms plutonic bodies with equal grain structure,including medium-fine diorite,monzonite,quartz monzonite and syenite; the second stage( 127 Ma) magmatism forms hypabyssal bodies,including porphyritic diorite and porphyritic quartz monzonite. Combined with field observation,petrography,mineralogy and geochemical characteristics,the petrogenesis of the Guzhen complex is analyzed. The Guzheng diorite has HMA properties. Guzhen diorite is a product of partial melting of the mantle peridotite metasomatized by the subduction slab melt and fluid,and the magma has weak assimilation and contamination with the crustal material on the ascending route. The Guzhen syenite is a product of partial melting of the thickened continental crust with the depth of 40 ～ 67 km. The Guzhen monzonite is formed by the mixing of syenite and diorite in the study area. The Guzhen quartz monzonite is formed by mixing of Guzhen diorite and another siliconrich magma. The subduction material( fluid + melt) has an important contribution to the formation of Guzheng high-Mg diorite,which shows that the influence of the subduction of the Paleo-Pacific plate also involves the central NCC,but the degree of the impact is less than that of the eastern NCC. The Guzhen syenite is formed by partial melting of the thickening continental crust,which shows that the delamination plays an important role in the thinning process of the NCC lithosphere in the Middle Mesozoic. Combined with the calculation results of the amphibole thermobarometer and the previous research results,it can be inferred that the time node of the large-scale delaminatiom of the central NCC is 127 Ma.
This paper takes the Guzhen intrusive complex which is located in Hebei Province in the central part of the North China Craton( NCC) as a research object. The author conducted detailed field geological survey,combined with indoor research,including petrography,mineralogy,geochemistry,Sr-Nd isotope,Lu-Hf isotope and U-Pb zircon chronology analysis,so as to explore the formation age,source area,petrogenesis of Guzhen intrusive complex,in order to draw new inspiration for the Mesozoic lithospheric thinning in the central NCC. In this paper,it is believed that the formation age of the Guzhen complex is related to the structure of the rock. The formation age of the rock with equal grain structure is earlier than that of the rock with porphyritic structure. Magmatic activity can be divided into two phases: the first stage( 130 ～ 135 Ma) magmatic activity forms plutonic bodies with equal grain structure,including medium-fine diorite,monzonite,quartz monzonite and syenite; the second stage( 127 Ma) magmatism forms hypabyssal bodies,including porphyritic diorite and porphyritic quartz monzonite. Combined with field observation,petrography,mineralogy and geochemical characteristics,the petrogenesis of the Guzhen complex is analyzed. The Guzheng diorite has HMA properties. Guzhen diorite is a product of partial melting of the mantle peridotite metasomatized by the subduction slab melt and fluid,and the magma has weak assimilation and contamination with the crustal material on the ascending route. The Guzhen syenite is a product of partial melting of the thickened continental crust with the depth of 40 ～ 67 km. The Guzhen monzonite is formed by the mixing of syenite and diorite in the study area. The Guzhen quartz monzonite is formed by mixing of Guzhen diorite and another siliconrich magma. The subduction material( fluid + melt) has an important contribution to the formation of Guzheng high-Mg diorite,which shows that the influence of the subduction of the Paleo-Pacific plate also involves the central NCC,but the degree of the impact is less than that of the eastern NCC. The Guzhen syenite is formed by partial melting of the thickening continental crust,which shows that the delamination plays an important role in the thinning process of the NCC lithosphere in the Middle Mesozoic. Combined with the calculation results of the amphibole thermobarometer and the previous research results,it can be inferred that the time node of the large-scale delaminatiom of the central NCC is 127 Ma.
引文
Barbarin B.1999.A review of the relationships between granitoid types,their origins and their geodynamic environments.Lithos,46:605-626
Black LP,Kamo SL,Allen CM,Aleinikoff JN,Davis DW,Korsch RJand Foudoulis C.2003.TEMORA 1:A new zircon standard for Phanerozoic U-Pb geochronology.Chemical Geology,200(1-2):155-170
Cai JH,Yan GH,Chang ZS,Wang XF,Shao HX and Chu ZY.2003.Petrological and geochemical characteristic of the Wanganzhen complex and discussion on its genesis.Acta Petrologica Sinica,19(1):81-92(in Chinese with English abstract)
Chen B,Tian W,Zhai MG and Arakawa Y.2005a.Zircon U-Pb geochronology and geochemistry of the Mesozoic magmatism in the Taihang Mountains and other places of the North China craton,with implications for petrogenesis and geodynamic setting.Acta Petrologica Sinica,21(1):13-24(in Chinese with English abstract)
Chen B,Zhai MG,Tian W and Jiang BM.2005b.Petrogenesis of the Mesozoic intrusive complexes from the southern Taihang Orogen,North China Craton:Elemental and Sr-Nd-Pb isotopic constraints.Bulletin of Mineralogy,Petrology and Geochemistry,24(2):93-102(in Chinese with English abstract)
Chen LH and Zhou XH.2005.Subduction-related metasomatism in the thinning Lithosphere:Evidence from a composite duniteorthopyroxenite xenolith entrained in Mesozoic Laiwu high-Mg diorite,North China Craton.Geochemistry,Geophysics,Geosystems,6(6):1-20
Condie KC.1973.Archean magmatism and crustal thickening.Geological Society of America Bulletin,84:2981-1992
Deng JF,Luo ZH,Su SG,Mo XX,Yu BS,Lai XY and Chen HW.2004.Rock Genesis,Tectonic Setting and Mineralization.Beijing:Geological Publishing House,26-28(in Chinese)
Deng JF,Su SG,Liu C,Zhao GC,Zhao XG,Zhou S and Wu ZX.2006.Discussion on the Lithospheric thinning of the North China craton:Delamination?or thermal erosion and chemical metasomatism?Earth Science Frontiers,13(2):105-119(in Chinese with English abstract)
Deng JF,Su SG,Niu YL,Liu C,Zhao GC,Zhao XG,Zhou S and Wu ZX.2007.A possible model for the lithospheric thinning of North China Craton:Evidence from the Yanshanian(Jura-Cretaceous)magmatism and tectonic deformation.Lithos,96:22-35
Fan WM,Zhang HF,Baker J,Jarvis KE,Mason PRD and Menzies MA.2000.On and off the North China Craton:Where is the Archaean keel.Journal of Petrology,41:933-950
Francis D and Ludden J.1995.The signature of amphibole in mafic alkaline lavas,a study in the Northern Canadian Cordillera.Journal of Petrology,36:1171-1191
Gao S,Rudnick RL,Carlson RW,Mcdonough WF and Liu YS.2002.Re-Os evidence for replacement of ancient mantle Lithosphere beneath the North China Craton.Earth and Planetary Science Letters,198:307-322
Gao S,Rudnick RL,Yuan HL,Liu XM,Liu YS,Xu WL,Ling WL,Ayers J,Wang XC and Wang QH.2004.Recycling lower continental crust in the North China Craton.Nature,432:892-897
Guo F,Fan WM,Wang YJ and Lin G.2001.Late Mesozoic mafic intrusive complexes in North China Block:Constraints on the nature of subcontinental lithospheric mantle.Physics and Chemistry of the Earth Part A Solid Earth and Geodesy,26(9-10):759-771
Guo F,Fan W,Wang YJ and Lin G.2003.Geochemistry of Late Mesozoic mafic magmatism in West Shandong Province,eastern China:Characterizing the lost lithospheric mantle beneath the North China Block.Geochemical Journal,37:63-77
Han YW and Ma ZD.2003.Geochemistry.Beijing:Geological Publishing House,203-204(in Chinese)
Hawkesworth CJ,Hergt JM,Ellam RM and Mc Dermott F.1991.Element fluxes associated with subduction related magmatism.Philosophical Transactions of the Royal Society of London.Series A:Physical and Engineering Sciences,335:393-405
Hermann J,Rubatto D,Korsakov A and Shatsky VS.2001.Multiple zircon growth during fast exhumation of diamondiferous,deeply subducted continental crust(Kokchetav massif,Kazakhstan).Contributions to Mineralogy and Petrology,141(1):66-82
Huo TF,Yang DB,Shi JP,Xu WL and Yang HT.2016.Petrogenesis of the Early Cretaceous alkali-rich intrusive rocks in the central North China Block:Constraints from zircon U-Pb chonology and Sr-Nd-Hf isotopes.Acta Petrologica Sinica,32(3):697-712(in Chinese with English abstract)
Kay RW and Kay SM.1993.Delamination and delamination magmatism.Tectonophys,219:177-189
Kelemen PB,Yogodzzinski GM and Scholl DW.2003.Along-strike variation in the Aleutian island arc:Genesis of high Mg#andesite and implications for continental crustal inside the subduction factory.American Geophysical Union Geophysical Monograph,138:223-276
Kelemen PB.1995.Genesis of high Mg-number andesites and the continental-crust.Contributions to Mineralogy and Petrology,120(1):1-19
Lesher CE.1990.Decoupling of chemical and isotopic exchange during magma mixing.Nature,344:235-237
Li CN and Liao QA.2006.Magmatic mixing and mingling of Precambrian Gangbian complex in northeastern Jiangxi Province and their geological significance.Acta Petrologica et Minerlogica,25(5):357-376(in Chinese with English abstract)
Li HY.2013.Destruction of North China Craton:Insights from temporal and spatial evolution of the proto-basins and magmatism.Scientia Sinica(Terrae),43(9):1396-1409(in Chinese)
Liu L,Chen B and Liu AK.2009.Petrogenesis of the Zijingguan mafic pluton,northern Taihang Orogen:Constraints from petrology and geochemistry.Earth Science,34(1):165-178(in Chinese with English abstract)
Liu SC and Xia QK.2014.Water content in the Early Cretaceous lithospheric mantle beneath the south-central Taihang Mountains:Implications for the destruction of the North China Craton.Chinese Science Bulletin,59:1280-1283(in Chinese)
Liu Y,Gao S,Kelemen PB and Xu W.2008.Recycled crust controls contrasting source compositions of Mesozoic and Cenozoic basalts in the North China Craton.Geochimica et Cosmochimica Acta,72:2349-2376
Luo ZH,Deng JF,Zhap GC and Cao YQ.1997.Magmatic activity characteristics of Taihangshan orogenic belt and its inversion of orogenic process.Earth Science,22(3):279-284(in Chinese with English abstract)
Ma CQ,Wang RJ and Qiu JX.1992.Signs of granitic magma origin and multiple magma mixing:Inclusions:Taking the Zhoukoudian rock mass in Beijing as an example.Geological Review,38(2):109-119(in Chinese with English abstract)
Martin H,Smithies RH,Rapp R,Moyen JF and Champion D.2005.An overview of adakite,tonalite-trondhjemite-granodiorite(TTG),and sanukitoid:Relationships and some implications for crustal evolution.Lithos,79(1-2):1-24
Mcdonough WF and Sun SS.1995.The composition of the Earth.Chemical Geology,120(3-4):223-253
Menzies MA,Fan WM and Zhang M.1993.Paleozoic and Cenozoic lithoprobe and the loss of>20km of Archean lithosphere,SinoKorean Craton,China.Geological Society,London,Special Publication,76:71-78
Menzies MA,Xu YG,Zhang H and Fan W.2007.Integration of geology,geophysics and geochemistry:A key to understanding the North China Craton.Lithos,96:1-21
Niu YL.2005.Generation and evolution of basaltic magmas:Some basic concepts and a hypothesis for the origin of the Mesozoic-Cenozoic volcanism in eastern China.Geological Journal of China Universities,11:9-46(in English with Chinese abstract)
Niu YL,Liu Y,Xue QQ,Shao FL,Chen S,Duan M,Guo PY,Gong HM,Hu Y,Hu ZH,Kong JJ,Li JY,Liu JJ,Sun P,Sun WL,Ye L,Xiao YY and Zhang Y.2015.Exotic origin of the Chinese continental shelf:New insights into the tectonic evolution of the western Pacific and eastern China since the Mesozoic.Earth Sciences,60(18):1598-1616
Pearce JA and Peate DW.1995.Tectonic implications of the composition of volcanic arc magmas.Annual Review of Earth and Planetary Sciences,23:251-285
Pearce JA.1996.Sources and setting of granitic rocks.Episodes,19(4):120-125
Pearson DG.1999.The age of continental roots.Lithos,48:171-194
Prouteau G,Scaillet B,Pichavant M and Maury R.2001.Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust.Nature,410:197-200
Qi L,Hu J and Gregoire DC.2000.Determination of trace elements in granites by inductively coupled plasma-mass spectrometry.Talanta,51(3):507-513
Qi Y,Luo JH,Wu JD and Chen FK 2016.Geochemical and Sr-Nd-Pb isotopic composition of the Canfang and Gufengshan granodiorite plutons in central-southern North China.Acta Petrologica Sinica,32(7):2015-2028(in Chinese with English abstract)
Rapp RP and Wastson EB.1995.Dehydration melting of metabasalt at 8~32kbar:Implications for continental growth and crust-mantle recycling.Journal of Petrology,36:891-931
Ridolfi F,Renzulli A and Puerini M.2010.Stability and chemical equilibrium of amphibole in calc-alkaline magmas:An overview,new thermobarometric formulations and application to subductionrelated volcanoes.Contributions to Mineralogy and Petrology,160:45-66
Schmidberger SS,Simonetti A,Francis D and Gariépy C.2002.Probing Archean Lithosphere using the Lu-Hf isotope systematics of peridotite xenoliths from Somerest Island kimberlites,Canada.Earth and Planetary Science Letters,197:245-259
Schmidt,Bottazzi P,Vannucci R and Mengel K.1999.Trace element partitioning between phlogopite,clinopyroxene and leucite lamproite melt.Earth and Planetary Science Letters,168:287-299
Su SG,Deng JF,Zhao GC,Zhao XG and Liu C.2006.Characteristics,origin and resource property of Xuejiashiliang complex,Beijing area and their relationship with the way of lithospheric thining.Earth Science Frontiers,13(2):148-157(in Chinese with English abstract)
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Sanders AD and Norry MJ(eds.).Magmatism in Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Sun Y.2016.Petrogenesis and Mineralization of the Early Cretaceous intrusive rocks in Handan-Xingtai area,Hebei Province,China.Ph.D.Dissertation.Beijing:China University of Geosciences,1-134(in Chinese with English summary)
Tatsumi Y and Ishizaka K.1982.Origin of high-magnesian andesites in the Setochi volcanic belt,Southwest Japan,Petrographical and chemical characteristics.Earth and Planetary Science Letters,60(2):293-304
Tatsumi Y and Nakamura N.1986.Composition of aquaeous fluid from serpentinite in the subducted lithosphere.Geochemical Journal,20:191-196
Tatsumi Y.1995.Subduction Zone Magmatism.Boston:Blackwell Publishing,1-244
Tatsumi Y.2001.Geochemical modeling of partial melting of subducting sediments and subsequent melt-mantle interaction:Generation of high-Mg andesites in the Setouchi volcanic belt,Southwest Japan.Geology,29(4):323-326
Taylor SR and Mc Lennan SM.1985.The Continental Crust:Its Composition and Evolution.Oxford:Blackwell Scientific Publications,1-312
Tepley FJ,Davidson JP,Tilling RI and Arth JG.2000.Magma mixing,recharge and eruption histories recorded in plagioclase phenocrysts from EI Chichon Volcano,Mexico.Journal of Petrology,41(9):1397-1411
Viccaro M,Giacomoni PP,Ferlito C and Cristofolini R.2010.Dynamics of magma supply at Mt.Etna volcano(Southern Italy)as revealed by textural and compositional features of plagioclase phenocrysts.Lithos,116(1-2):77-91
Wang DZ and Xie L.2008.Magma Mingling:Evidence from Enclaves.Geological Journal of China Universities 14(1):16-21(in Chinese with English abstract)
Wang T.2000.Origin of hybrid granitoids and the implications for continental dynamics.Acta Petrologica Sinica,16(2):161-168(in Chinese with English abstract)
Wang XX,Wang T,Lu XX and Xiao QH.2002.Petrographic evidence of the magmatic mixing of Laojunshan and Qinling Lianghuan granitoids in the North Qinling Mountains and its significance.Geological Bulletin of China,24(8-9):523-529(in Chinese with English abstract)
Wang Y.2018.Origin and formation mechanism of pyroxene syenite in Hongshan,Xishimen,Hebei Province.Master Degree Thesis.Beijing:China University of Geosciences,1-83(in Chinese with English summary)
Weaver BL and Tarney J.1984.Empirical approach to estimating the composition of the continental crust.Nature,310(5978):575-577
Wolf MB and Wyllie PJ.1992.The formation of tonalitic liquids during the vapor-absent partial melting of amphibolite at 10kbar.Eos,70:506-518
Wu FY,Lin JQ,Wilde SA,Zhang XO and Yang JH.2005.Nature and significance of the Early Cretaceous giant igneous event in eastern China.Earth and Planetary Science Letters,233:103-119
Wu FY,Li XH,Zheng YF and Gao S.2007.Lu-Hf isotopic systematics and their applications in petrology.Acta Petroloica Sinica,23(2):185-220(in Chinese with English abstract)
Wu FY,Xu YG,Gao S and Zheng JP.2008.Lithospheric thining and destruction of North China Craton.Acta Petroloica Sinica,24(6):1145-1174(in Chinese with English abstract)
Wyllie PJ,Cox KG and Biggar GM.1962.The habit of apatite in synthetic systems and igneous rocks.Journal of Petrology,3(2):238-243
Xia QK and Hao YT.2013.The distribution of water in the continental Lithospheric mantle and its implications for the stability of continents.Chinese Science Bulletin,58:3879-3889
Xia QK,Cheng H and Liu J.2017.The distribution of the Early Cretaceous hydrous lithophere mantla in the North China Ctaton:Constraints from water content in peridotites of Tietonggou.Earth Science,42(6):853-861(in Chinese with English abstract)
Xu JF,Shinjo R,Defant MJ,Wang Q,and Rapp RP.2002.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of East China:Partial melting of delaminated lower continental crust.Geology,30(12):1111-1114
Xu W,Hergt JM,Gao S,Pei F,Wang W and Yang D.2008.Interaction of adakitic melt-peridotite:Implications for the high-Mg#signature of Mesozoic adakitic rocks in the eastern China Craton.Earth and Planetary Science Letters,265(1-2):123-137
Xu WL,Wang QH,Wang DY,Pei FP and Gao S.2004.Processes and mechanism of Mesozoic lithospheric thinning in eastern North China Craton:Evidence from Mesozoic igneous rocks and deep-seated xenoliths.Earth Science Frontiers,11(3):310-317(in Chinese with English abstract)
Xu WL,Yang DB,Pei FP and Yu Y.2009.Petrogenesis of Fushan high-Mg#diorites from the southern Taihang Mts.in the central North China Craton:Resulting from interaction of peridotite-melt derived from partial melting of delamination lower continental crust.Acta Petrologica Sinica,25(8):1947-1961(in Chinese with English abstract)
Xu YG,Huang XL,Ma JL,Wang YB,Lizuka Y,Xu JF,Wang Q and Wu XY.2004.Crust-mantle interaction during the tectono-thermal reactivation of the North China craton:Constraints from SHRIMPzircon U-Pb chronology and geochemistry of Mesozoic plutons from western Shandong.Contributions to Mineralogy and Petrology,147:750-767
Yang CH,Xu WL,Yang DB,Wang W,Wang WD and Liu JM.2008.Petrogenesis of Shangyu gabbro-diorites in the west of Shandong:Evidence of chronology and geochemistry.Science in China(Series D),38(1):44-55(in Chinese)
Yang JH,Chung SL,Zhai MG and Zhou XH.2004.Geochemical and Sr-Nd-Pb isotopic compositions of mafic dikes from the Jiaodong Peninsula,China:Evidence for vein-plus-peridotite melting in the lithospheric mantle.Lithos,73:145-160
Yang JH,Sun JF and Chen FK.2007.Sources and petrogenesis of Late Triassic dolerite dikes in the Liaodong Peninsula:Implications for post-collisional Lithosphere thinning of eastern North China craton.Journal of Petrology,48:1973-1997
Yin JY,Yuan C,Sun M,Long XP,Zhao GC,Wong KP,Geng HY and Cai KD.2010.Late Carboniferous high-Mg dioritic dikes in western Junggar,NW China:Geochemical features,petrogenesis and tectonic implications.Gondwana Research,17:145-152
Ying JF,Zhou XH and Zhang HF.2004.Geochemical and isotopic investigation of the Laiwu-Zibo carbonatites from western Shandong Province,China,and implications for their petrogenesis and enriched mantle source.Lithos,75:413-426
Zhang HF,Sun M,Zhou XH,Zhou XH,Fan WM,Zhai MG and Yin JF.2002.Mesozoic Lithosphere destruction beneath the North China Craton:Evidence from major,trace element,and Sr-Nd-Pb isotope studies of Fangcheng basalts.Contributions to Mineralogy and Petrology,144:241-253
Zhang HF,Sun YL,Tang YJ,Xiao Y,Zhang WH,Zhao XM,Santosh M and Menzies MA.2012.Melt peridotite interaction in the PreCambrian mantle beneath the western North China Craton:Petrology,geochemistry and Sr,Nd and Re isotopes.Lithos,149:100-114
Zhang Q,Wang Y,Li CD,Wang YL,Jin WJ and Jia XQ.2006.Granite classification on the basis of Sr and Yb contents and its implications.Acta Petrologica Sinica,22(9):2249-2269(in Chinese with English abstract)
Zhang Q,Wang Y,Xiong XL and Li CD.2008.Adakite and Granite Challenge and Opportunity.Beijing:China Land Press,107-129(in Chinese)
Zhang SH,Zhao Y,Liu XC,Liu DY,Chen FK,Xie LW and Chen HH.2009.Late Paleozoic to Early Mesozoic mafic-ultramafic complexes from the northern North China block:Constraints on the composition and evolution of the lithospheric mantle.Lithos,110:229-246
Zhao GC,Sun M and Wilde SA.2002.Characteristics of the basement tectonic units of the North China Craton and the Early Proterozoic colliding.Science in China(Series D),32:538-549(in Chinese)
Zhao Y,Chen B,Zhang SH,Liu JM,Hu JM,Liu J and Pei JL.2010.Major geological events in the northern margin of the North China Craton and the adjacent area in Early Yanshan Period.Geology in China,37(4):900-915(in Chinese with English abstract)
Zheng JP,Lu FX,O’Reilly SY,Griffin WL and Zhang M.1999.Characteristics and evolution of the Paleozoic and Cenozoic lithospheric mantles in the eastern North China Platform.Acta Geologica Sinica,73(1):47-56(in Chinese with English abstract)
Zhou R and Wu KL.1994.Zhangzhou I-A type granite.Beijing:Science Press,1-152(in Chinese)
Zhu RX,Chen L,Wu FY and Liu JL.2011.Timing,scale and mechanism of the destruction of the North China Craton.Scientia Sinica(Terrae),41(5):583-592(in Chinese)
蔡剑辉,闫国翰,常兆山,王晓芳,邵宏翔,储著银.2003.王安镇岩体岩石地球化学特征及成因探讨.岩石学报,19(1):81-92
陈斌,田伟,翟明国,荒川洋二.2005a.太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义.岩石学报,21(1):13-24
陈斌,翟明国,田伟,江博明.2005b.太行山南段中生代杂岩体的岩石成因:元素和Nd-Sr-Pb同位素地球化学证据.矿物岩石地球化学通报,24(2):93-102
邓晋福,罗照华,苏尚国,莫宣学,于炳松,赖兴运,谌宏伟.2004.岩石成因、构造环境与成矿作用.北京:地质出版社,26-28
邓晋福,苏尚国,刘翠,赵国春,赵兴国,周肃,吴宗絮.2006.关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论:是拆沉,还是热侵蚀和化学交代?地学前缘,(2):105-119
韩吟文,马振东.2003.地球化学.北京:地质出版社,203-204
霍腾飞,杨德彬,师江朋,许文良,杨浩田.2016.华北地块中部早白垩世富碱侵入岩的成因:锆石U-Pb年代学和Sr-Nd-Hf同位素制约.岩石学报,32(3):697-712
李昌年,廖群安.2006.赣东北前寒武纪港边杂岩体的岩浆混合(和)作用及其地质意义.岩石矿物学杂志,25(5):357-376
李洪颜.2013.华北克拉通原型盆地及岩浆活动时空演化对克拉通破坏的制约.中国科学(地球科学),43(9):1396-1409
刘玲,陈斌,刘安坤.2009.北太行紫荆关基性岩体的成因:岩石学和地球化学的证据.地球科学,34(1):165-178
刘少辰,夏群科.2014.太行山中南段早白垩世岩石圈地幔的水含量:对华北克拉通破坏的动力因素制约.科学通报,59:1280-1283
罗照华,邓晋福,赵国春,曹永清.1997.太行山造山带岩浆活动特征及其造山过程反演.地球科学,22(3):279-284
马昌前,王人镜,邱家骧.1992.花岗质岩浆起源和多次岩浆混合的标志:包体---以北京周口店岩体为例.地质论评,38(2):109-119
齐玥,罗金海,巫嘉德,陈福坤.2016.华北中南部蚕坊和孤峰山花岗闪长岩岩体的地球化学特征和Sr-Nd-Pb同位素组成.岩石学报,32(7):2015-2028
苏尚国,邓晋福,赵国春,赵兴国,刘翠.2006.北京燕山地区薛家石梁杂岩体特征、成因、源区性质及岩石圈减薄方式.地学前缘,13(2):148-157
孙熠.2016.河北邯邢地区早白垩世岩浆作用及成矿意义.博士学位论文.北京:中国地质大学,1-134
王德滋,谢磊.2008.岩浆混合作用:来自岩石包体的证据.高校地质学报,14(1):16-21
王涛.2000.花岗岩混合成因研究及大陆动力学意义.岩石学报,16(2):161-168
王晓霞,王涛,卢欣祥,肖庆辉.2002.北秦岭老君山、秦岭梁环斑结构花岗岩岩浆混合的岩相学证据及其意义.地质通报,24(8-9):523-529
王玉.2018.河北武安西石门洪山辉石正长岩的成因和形成机制.硕士学位论文.北京:中国地质大学,1-83
吴福元,李献华,郑永飞,高山.2007.Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220
吴福元,徐义刚,高山,郑建平.2008.华北岩石圈减薄与克拉通破坏研究的主要学术争论.岩石学报,24(6):1145-1174
谢群科,程徽,刘佳.2017.山东铁铜沟橄榄岩的水含量:华北克拉通早白垩世富水岩石圈的分布.地球科学,42(6):853-861
许文良,王清海,王冬艳,裴福萍,高山.2004.华北克拉通东部中生代岩石圈减薄的过程与机制:中生代火成岩和深源捕虏体证据.地学前缘,11(3):310-317
许文良,杨德彬,裴福萍,于洋.2009.太行山南段符山高镁闪长岩的成因---拆沉陆壳物质熔融的熔体与地幔橄榄岩反应的结果.岩石学报,25(8):1947-1961
杨承海,许文良,杨德彬,王伟,王伟德,刘金民.2008.鲁西上峪辉长-闪长岩的成因:年代学与岩石地球化学证据中国科学(D辑),38(1):44-55
张旗,王焰,李承东,王元龙,金惟俊,贾秀勤.2006.花岗岩的Sr-Yb分类及其地质意义.岩石学报,22(9):2249-2269
张旗,王焰,熊小林,李承东.2008.埃达克岩和花岗岩:挑战和机遇.北京:中国大地出版社,107-129
赵国春,孙敏,Wilde SA.2002.华北克拉通基底构造单元特征及早元古代拼合.中国科学(D辑),32:538-549
赵越,陈斌,张拴宏,刘建民,胡健民,刘健,裴军令.2010.华北克拉通北缘及邻区前燕山期主要地质事件.中国地质,37(4):900-915
郑建平,路凤祥,Reilly SYO,Griffin WL,张明.1999.华北地台东部古生代与新生代岩石圈地幔特征及其演化.地质学报,73(1):47-56
周珣若,吴克隆.1994.漳州I-A型花岗岩.北京:科学出版社,1-152
朱日祥,陈凌,吴福元,刘俊来.2011.华北克拉通破坏的时间、范围与机制.中国科学(地球科学),41(5):583-592
Black LP,Kamo SL,Allen CM,Aleinikoff JN,Davis DW,Korsch RJand Foudoulis C.2003.TEMORA 1:A new zircon standard for Phanerozoic U-Pb geochronology.Chemical Geology,200(1-2):155-170
Cai JH,Yan GH,Chang ZS,Wang XF,Shao HX and Chu ZY.2003.Petrological and geochemical characteristic of the Wanganzhen complex and discussion on its genesis.Acta Petrologica Sinica,19(1):81-92(in Chinese with English abstract)
Chen B,Tian W,Zhai MG and Arakawa Y.2005a.Zircon U-Pb geochronology and geochemistry of the Mesozoic magmatism in the Taihang Mountains and other places of the North China craton,with implications for petrogenesis and geodynamic setting.Acta Petrologica Sinica,21(1):13-24(in Chinese with English abstract)
Chen B,Zhai MG,Tian W and Jiang BM.2005b.Petrogenesis of the Mesozoic intrusive complexes from the southern Taihang Orogen,North China Craton:Elemental and Sr-Nd-Pb isotopic constraints.Bulletin of Mineralogy,Petrology and Geochemistry,24(2):93-102(in Chinese with English abstract)
Chen LH and Zhou XH.2005.Subduction-related metasomatism in the thinning Lithosphere:Evidence from a composite duniteorthopyroxenite xenolith entrained in Mesozoic Laiwu high-Mg diorite,North China Craton.Geochemistry,Geophysics,Geosystems,6(6):1-20
Condie KC.1973.Archean magmatism and crustal thickening.Geological Society of America Bulletin,84:2981-1992
Deng JF,Luo ZH,Su SG,Mo XX,Yu BS,Lai XY and Chen HW.2004.Rock Genesis,Tectonic Setting and Mineralization.Beijing:Geological Publishing House,26-28(in Chinese)
Deng JF,Su SG,Liu C,Zhao GC,Zhao XG,Zhou S and Wu ZX.2006.Discussion on the Lithospheric thinning of the North China craton:Delamination?or thermal erosion and chemical metasomatism?Earth Science Frontiers,13(2):105-119(in Chinese with English abstract)
Deng JF,Su SG,Niu YL,Liu C,Zhao GC,Zhao XG,Zhou S and Wu ZX.2007.A possible model for the lithospheric thinning of North China Craton:Evidence from the Yanshanian(Jura-Cretaceous)magmatism and tectonic deformation.Lithos,96:22-35
Fan WM,Zhang HF,Baker J,Jarvis KE,Mason PRD and Menzies MA.2000.On and off the North China Craton:Where is the Archaean keel.Journal of Petrology,41:933-950
Francis D and Ludden J.1995.The signature of amphibole in mafic alkaline lavas,a study in the Northern Canadian Cordillera.Journal of Petrology,36:1171-1191
Gao S,Rudnick RL,Carlson RW,Mcdonough WF and Liu YS.2002.Re-Os evidence for replacement of ancient mantle Lithosphere beneath the North China Craton.Earth and Planetary Science Letters,198:307-322
Gao S,Rudnick RL,Yuan HL,Liu XM,Liu YS,Xu WL,Ling WL,Ayers J,Wang XC and Wang QH.2004.Recycling lower continental crust in the North China Craton.Nature,432:892-897
Guo F,Fan WM,Wang YJ and Lin G.2001.Late Mesozoic mafic intrusive complexes in North China Block:Constraints on the nature of subcontinental lithospheric mantle.Physics and Chemistry of the Earth Part A Solid Earth and Geodesy,26(9-10):759-771
Guo F,Fan W,Wang YJ and Lin G.2003.Geochemistry of Late Mesozoic mafic magmatism in West Shandong Province,eastern China:Characterizing the lost lithospheric mantle beneath the North China Block.Geochemical Journal,37:63-77
Han YW and Ma ZD.2003.Geochemistry.Beijing:Geological Publishing House,203-204(in Chinese)
Hawkesworth CJ,Hergt JM,Ellam RM and Mc Dermott F.1991.Element fluxes associated with subduction related magmatism.Philosophical Transactions of the Royal Society of London.Series A:Physical and Engineering Sciences,335:393-405
Hermann J,Rubatto D,Korsakov A and Shatsky VS.2001.Multiple zircon growth during fast exhumation of diamondiferous,deeply subducted continental crust(Kokchetav massif,Kazakhstan).Contributions to Mineralogy and Petrology,141(1):66-82
Huo TF,Yang DB,Shi JP,Xu WL and Yang HT.2016.Petrogenesis of the Early Cretaceous alkali-rich intrusive rocks in the central North China Block:Constraints from zircon U-Pb chonology and Sr-Nd-Hf isotopes.Acta Petrologica Sinica,32(3):697-712(in Chinese with English abstract)
Kay RW and Kay SM.1993.Delamination and delamination magmatism.Tectonophys,219:177-189
Kelemen PB,Yogodzzinski GM and Scholl DW.2003.Along-strike variation in the Aleutian island arc:Genesis of high Mg#andesite and implications for continental crustal inside the subduction factory.American Geophysical Union Geophysical Monograph,138:223-276
Kelemen PB.1995.Genesis of high Mg-number andesites and the continental-crust.Contributions to Mineralogy and Petrology,120(1):1-19
Lesher CE.1990.Decoupling of chemical and isotopic exchange during magma mixing.Nature,344:235-237
Li CN and Liao QA.2006.Magmatic mixing and mingling of Precambrian Gangbian complex in northeastern Jiangxi Province and their geological significance.Acta Petrologica et Minerlogica,25(5):357-376(in Chinese with English abstract)
Li HY.2013.Destruction of North China Craton:Insights from temporal and spatial evolution of the proto-basins and magmatism.Scientia Sinica(Terrae),43(9):1396-1409(in Chinese)
Liu L,Chen B and Liu AK.2009.Petrogenesis of the Zijingguan mafic pluton,northern Taihang Orogen:Constraints from petrology and geochemistry.Earth Science,34(1):165-178(in Chinese with English abstract)
Liu SC and Xia QK.2014.Water content in the Early Cretaceous lithospheric mantle beneath the south-central Taihang Mountains:Implications for the destruction of the North China Craton.Chinese Science Bulletin,59:1280-1283(in Chinese)
Liu Y,Gao S,Kelemen PB and Xu W.2008.Recycled crust controls contrasting source compositions of Mesozoic and Cenozoic basalts in the North China Craton.Geochimica et Cosmochimica Acta,72:2349-2376
Luo ZH,Deng JF,Zhap GC and Cao YQ.1997.Magmatic activity characteristics of Taihangshan orogenic belt and its inversion of orogenic process.Earth Science,22(3):279-284(in Chinese with English abstract)
Ma CQ,Wang RJ and Qiu JX.1992.Signs of granitic magma origin and multiple magma mixing:Inclusions:Taking the Zhoukoudian rock mass in Beijing as an example.Geological Review,38(2):109-119(in Chinese with English abstract)
Martin H,Smithies RH,Rapp R,Moyen JF and Champion D.2005.An overview of adakite,tonalite-trondhjemite-granodiorite(TTG),and sanukitoid:Relationships and some implications for crustal evolution.Lithos,79(1-2):1-24
Mcdonough WF and Sun SS.1995.The composition of the Earth.Chemical Geology,120(3-4):223-253
Menzies MA,Fan WM and Zhang M.1993.Paleozoic and Cenozoic lithoprobe and the loss of>20km of Archean lithosphere,SinoKorean Craton,China.Geological Society,London,Special Publication,76:71-78
Menzies MA,Xu YG,Zhang H and Fan W.2007.Integration of geology,geophysics and geochemistry:A key to understanding the North China Craton.Lithos,96:1-21
Niu YL.2005.Generation and evolution of basaltic magmas:Some basic concepts and a hypothesis for the origin of the Mesozoic-Cenozoic volcanism in eastern China.Geological Journal of China Universities,11:9-46(in English with Chinese abstract)
Niu YL,Liu Y,Xue QQ,Shao FL,Chen S,Duan M,Guo PY,Gong HM,Hu Y,Hu ZH,Kong JJ,Li JY,Liu JJ,Sun P,Sun WL,Ye L,Xiao YY and Zhang Y.2015.Exotic origin of the Chinese continental shelf:New insights into the tectonic evolution of the western Pacific and eastern China since the Mesozoic.Earth Sciences,60(18):1598-1616
Pearce JA and Peate DW.1995.Tectonic implications of the composition of volcanic arc magmas.Annual Review of Earth and Planetary Sciences,23:251-285
Pearce JA.1996.Sources and setting of granitic rocks.Episodes,19(4):120-125
Pearson DG.1999.The age of continental roots.Lithos,48:171-194
Prouteau G,Scaillet B,Pichavant M and Maury R.2001.Evidence for mantle metasomatism by hydrous silicic melts derived from subducted oceanic crust.Nature,410:197-200
Qi L,Hu J and Gregoire DC.2000.Determination of trace elements in granites by inductively coupled plasma-mass spectrometry.Talanta,51(3):507-513
Qi Y,Luo JH,Wu JD and Chen FK 2016.Geochemical and Sr-Nd-Pb isotopic composition of the Canfang and Gufengshan granodiorite plutons in central-southern North China.Acta Petrologica Sinica,32(7):2015-2028(in Chinese with English abstract)
Rapp RP and Wastson EB.1995.Dehydration melting of metabasalt at 8~32kbar:Implications for continental growth and crust-mantle recycling.Journal of Petrology,36:891-931
Ridolfi F,Renzulli A and Puerini M.2010.Stability and chemical equilibrium of amphibole in calc-alkaline magmas:An overview,new thermobarometric formulations and application to subductionrelated volcanoes.Contributions to Mineralogy and Petrology,160:45-66
Schmidberger SS,Simonetti A,Francis D and Gariépy C.2002.Probing Archean Lithosphere using the Lu-Hf isotope systematics of peridotite xenoliths from Somerest Island kimberlites,Canada.Earth and Planetary Science Letters,197:245-259
Schmidt,Bottazzi P,Vannucci R and Mengel K.1999.Trace element partitioning between phlogopite,clinopyroxene and leucite lamproite melt.Earth and Planetary Science Letters,168:287-299
Su SG,Deng JF,Zhao GC,Zhao XG and Liu C.2006.Characteristics,origin and resource property of Xuejiashiliang complex,Beijing area and their relationship with the way of lithospheric thining.Earth Science Frontiers,13(2):148-157(in Chinese with English abstract)
Sun SS and Mc Donough WF.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes.In:Sanders AD and Norry MJ(eds.).Magmatism in Ocean Basins.Geological Society,London,Special Publication,42(1):313-345
Sun Y.2016.Petrogenesis and Mineralization of the Early Cretaceous intrusive rocks in Handan-Xingtai area,Hebei Province,China.Ph.D.Dissertation.Beijing:China University of Geosciences,1-134(in Chinese with English summary)
Tatsumi Y and Ishizaka K.1982.Origin of high-magnesian andesites in the Setochi volcanic belt,Southwest Japan,Petrographical and chemical characteristics.Earth and Planetary Science Letters,60(2):293-304
Tatsumi Y and Nakamura N.1986.Composition of aquaeous fluid from serpentinite in the subducted lithosphere.Geochemical Journal,20:191-196
Tatsumi Y.1995.Subduction Zone Magmatism.Boston:Blackwell Publishing,1-244
Tatsumi Y.2001.Geochemical modeling of partial melting of subducting sediments and subsequent melt-mantle interaction:Generation of high-Mg andesites in the Setouchi volcanic belt,Southwest Japan.Geology,29(4):323-326
Taylor SR and Mc Lennan SM.1985.The Continental Crust:Its Composition and Evolution.Oxford:Blackwell Scientific Publications,1-312
Tepley FJ,Davidson JP,Tilling RI and Arth JG.2000.Magma mixing,recharge and eruption histories recorded in plagioclase phenocrysts from EI Chichon Volcano,Mexico.Journal of Petrology,41(9):1397-1411
Viccaro M,Giacomoni PP,Ferlito C and Cristofolini R.2010.Dynamics of magma supply at Mt.Etna volcano(Southern Italy)as revealed by textural and compositional features of plagioclase phenocrysts.Lithos,116(1-2):77-91
Wang DZ and Xie L.2008.Magma Mingling:Evidence from Enclaves.Geological Journal of China Universities 14(1):16-21(in Chinese with English abstract)
Wang T.2000.Origin of hybrid granitoids and the implications for continental dynamics.Acta Petrologica Sinica,16(2):161-168(in Chinese with English abstract)
Wang XX,Wang T,Lu XX and Xiao QH.2002.Petrographic evidence of the magmatic mixing of Laojunshan and Qinling Lianghuan granitoids in the North Qinling Mountains and its significance.Geological Bulletin of China,24(8-9):523-529(in Chinese with English abstract)
Wang Y.2018.Origin and formation mechanism of pyroxene syenite in Hongshan,Xishimen,Hebei Province.Master Degree Thesis.Beijing:China University of Geosciences,1-83(in Chinese with English summary)
Weaver BL and Tarney J.1984.Empirical approach to estimating the composition of the continental crust.Nature,310(5978):575-577
Wolf MB and Wyllie PJ.1992.The formation of tonalitic liquids during the vapor-absent partial melting of amphibolite at 10kbar.Eos,70:506-518
Wu FY,Lin JQ,Wilde SA,Zhang XO and Yang JH.2005.Nature and significance of the Early Cretaceous giant igneous event in eastern China.Earth and Planetary Science Letters,233:103-119
Wu FY,Li XH,Zheng YF and Gao S.2007.Lu-Hf isotopic systematics and their applications in petrology.Acta Petroloica Sinica,23(2):185-220(in Chinese with English abstract)
Wu FY,Xu YG,Gao S and Zheng JP.2008.Lithospheric thining and destruction of North China Craton.Acta Petroloica Sinica,24(6):1145-1174(in Chinese with English abstract)
Wyllie PJ,Cox KG and Biggar GM.1962.The habit of apatite in synthetic systems and igneous rocks.Journal of Petrology,3(2):238-243
Xia QK and Hao YT.2013.The distribution of water in the continental Lithospheric mantle and its implications for the stability of continents.Chinese Science Bulletin,58:3879-3889
Xia QK,Cheng H and Liu J.2017.The distribution of the Early Cretaceous hydrous lithophere mantla in the North China Ctaton:Constraints from water content in peridotites of Tietonggou.Earth Science,42(6):853-861(in Chinese with English abstract)
Xu JF,Shinjo R,Defant MJ,Wang Q,and Rapp RP.2002.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of East China:Partial melting of delaminated lower continental crust.Geology,30(12):1111-1114
Xu W,Hergt JM,Gao S,Pei F,Wang W and Yang D.2008.Interaction of adakitic melt-peridotite:Implications for the high-Mg#signature of Mesozoic adakitic rocks in the eastern China Craton.Earth and Planetary Science Letters,265(1-2):123-137
Xu WL,Wang QH,Wang DY,Pei FP and Gao S.2004.Processes and mechanism of Mesozoic lithospheric thinning in eastern North China Craton:Evidence from Mesozoic igneous rocks and deep-seated xenoliths.Earth Science Frontiers,11(3):310-317(in Chinese with English abstract)
Xu WL,Yang DB,Pei FP and Yu Y.2009.Petrogenesis of Fushan high-Mg#diorites from the southern Taihang Mts.in the central North China Craton:Resulting from interaction of peridotite-melt derived from partial melting of delamination lower continental crust.Acta Petrologica Sinica,25(8):1947-1961(in Chinese with English abstract)
Xu YG,Huang XL,Ma JL,Wang YB,Lizuka Y,Xu JF,Wang Q and Wu XY.2004.Crust-mantle interaction during the tectono-thermal reactivation of the North China craton:Constraints from SHRIMPzircon U-Pb chronology and geochemistry of Mesozoic plutons from western Shandong.Contributions to Mineralogy and Petrology,147:750-767
Yang CH,Xu WL,Yang DB,Wang W,Wang WD and Liu JM.2008.Petrogenesis of Shangyu gabbro-diorites in the west of Shandong:Evidence of chronology and geochemistry.Science in China(Series D),38(1):44-55(in Chinese)
Yang JH,Chung SL,Zhai MG and Zhou XH.2004.Geochemical and Sr-Nd-Pb isotopic compositions of mafic dikes from the Jiaodong Peninsula,China:Evidence for vein-plus-peridotite melting in the lithospheric mantle.Lithos,73:145-160
Yang JH,Sun JF and Chen FK.2007.Sources and petrogenesis of Late Triassic dolerite dikes in the Liaodong Peninsula:Implications for post-collisional Lithosphere thinning of eastern North China craton.Journal of Petrology,48:1973-1997
Yin JY,Yuan C,Sun M,Long XP,Zhao GC,Wong KP,Geng HY and Cai KD.2010.Late Carboniferous high-Mg dioritic dikes in western Junggar,NW China:Geochemical features,petrogenesis and tectonic implications.Gondwana Research,17:145-152
Ying JF,Zhou XH and Zhang HF.2004.Geochemical and isotopic investigation of the Laiwu-Zibo carbonatites from western Shandong Province,China,and implications for their petrogenesis and enriched mantle source.Lithos,75:413-426
Zhang HF,Sun M,Zhou XH,Zhou XH,Fan WM,Zhai MG and Yin JF.2002.Mesozoic Lithosphere destruction beneath the North China Craton:Evidence from major,trace element,and Sr-Nd-Pb isotope studies of Fangcheng basalts.Contributions to Mineralogy and Petrology,144:241-253
Zhang HF,Sun YL,Tang YJ,Xiao Y,Zhang WH,Zhao XM,Santosh M and Menzies MA.2012.Melt peridotite interaction in the PreCambrian mantle beneath the western North China Craton:Petrology,geochemistry and Sr,Nd and Re isotopes.Lithos,149:100-114
Zhang Q,Wang Y,Li CD,Wang YL,Jin WJ and Jia XQ.2006.Granite classification on the basis of Sr and Yb contents and its implications.Acta Petrologica Sinica,22(9):2249-2269(in Chinese with English abstract)
Zhang Q,Wang Y,Xiong XL and Li CD.2008.Adakite and Granite Challenge and Opportunity.Beijing:China Land Press,107-129(in Chinese)
Zhang SH,Zhao Y,Liu XC,Liu DY,Chen FK,Xie LW and Chen HH.2009.Late Paleozoic to Early Mesozoic mafic-ultramafic complexes from the northern North China block:Constraints on the composition and evolution of the lithospheric mantle.Lithos,110:229-246
Zhao GC,Sun M and Wilde SA.2002.Characteristics of the basement tectonic units of the North China Craton and the Early Proterozoic colliding.Science in China(Series D),32:538-549(in Chinese)
Zhao Y,Chen B,Zhang SH,Liu JM,Hu JM,Liu J and Pei JL.2010.Major geological events in the northern margin of the North China Craton and the adjacent area in Early Yanshan Period.Geology in China,37(4):900-915(in Chinese with English abstract)
Zheng JP,Lu FX,O’Reilly SY,Griffin WL and Zhang M.1999.Characteristics and evolution of the Paleozoic and Cenozoic lithospheric mantles in the eastern North China Platform.Acta Geologica Sinica,73(1):47-56(in Chinese with English abstract)
Zhou R and Wu KL.1994.Zhangzhou I-A type granite.Beijing:Science Press,1-152(in Chinese)
Zhu RX,Chen L,Wu FY and Liu JL.2011.Timing,scale and mechanism of the destruction of the North China Craton.Scientia Sinica(Terrae),41(5):583-592(in Chinese)
蔡剑辉,闫国翰,常兆山,王晓芳,邵宏翔,储著银.2003.王安镇岩体岩石地球化学特征及成因探讨.岩石学报,19(1):81-92
陈斌,田伟,翟明国,荒川洋二.2005a.太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义.岩石学报,21(1):13-24
陈斌,翟明国,田伟,江博明.2005b.太行山南段中生代杂岩体的岩石成因:元素和Nd-Sr-Pb同位素地球化学证据.矿物岩石地球化学通报,24(2):93-102
邓晋福,罗照华,苏尚国,莫宣学,于炳松,赖兴运,谌宏伟.2004.岩石成因、构造环境与成矿作用.北京:地质出版社,26-28
邓晋福,苏尚国,刘翠,赵国春,赵兴国,周肃,吴宗絮.2006.关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论:是拆沉,还是热侵蚀和化学交代?地学前缘,(2):105-119
韩吟文,马振东.2003.地球化学.北京:地质出版社,203-204
霍腾飞,杨德彬,师江朋,许文良,杨浩田.2016.华北地块中部早白垩世富碱侵入岩的成因:锆石U-Pb年代学和Sr-Nd-Hf同位素制约.岩石学报,32(3):697-712
李昌年,廖群安.2006.赣东北前寒武纪港边杂岩体的岩浆混合(和)作用及其地质意义.岩石矿物学杂志,25(5):357-376
李洪颜.2013.华北克拉通原型盆地及岩浆活动时空演化对克拉通破坏的制约.中国科学(地球科学),43(9):1396-1409
刘玲,陈斌,刘安坤.2009.北太行紫荆关基性岩体的成因:岩石学和地球化学的证据.地球科学,34(1):165-178
刘少辰,夏群科.2014.太行山中南段早白垩世岩石圈地幔的水含量:对华北克拉通破坏的动力因素制约.科学通报,59:1280-1283
罗照华,邓晋福,赵国春,曹永清.1997.太行山造山带岩浆活动特征及其造山过程反演.地球科学,22(3):279-284
马昌前,王人镜,邱家骧.1992.花岗质岩浆起源和多次岩浆混合的标志:包体---以北京周口店岩体为例.地质论评,38(2):109-119
齐玥,罗金海,巫嘉德,陈福坤.2016.华北中南部蚕坊和孤峰山花岗闪长岩岩体的地球化学特征和Sr-Nd-Pb同位素组成.岩石学报,32(7):2015-2028
苏尚国,邓晋福,赵国春,赵兴国,刘翠.2006.北京燕山地区薛家石梁杂岩体特征、成因、源区性质及岩石圈减薄方式.地学前缘,13(2):148-157
孙熠.2016.河北邯邢地区早白垩世岩浆作用及成矿意义.博士学位论文.北京:中国地质大学,1-134
王德滋,谢磊.2008.岩浆混合作用:来自岩石包体的证据.高校地质学报,14(1):16-21
王涛.2000.花岗岩混合成因研究及大陆动力学意义.岩石学报,16(2):161-168
王晓霞,王涛,卢欣祥,肖庆辉.2002.北秦岭老君山、秦岭梁环斑结构花岗岩岩浆混合的岩相学证据及其意义.地质通报,24(8-9):523-529
王玉.2018.河北武安西石门洪山辉石正长岩的成因和形成机制.硕士学位论文.北京:中国地质大学,1-83
吴福元,李献华,郑永飞,高山.2007.Lu-Hf同位素体系及其岩石学应用.岩石学报,23(2):185-220
吴福元,徐义刚,高山,郑建平.2008.华北岩石圈减薄与克拉通破坏研究的主要学术争论.岩石学报,24(6):1145-1174
谢群科,程徽,刘佳.2017.山东铁铜沟橄榄岩的水含量:华北克拉通早白垩世富水岩石圈的分布.地球科学,42(6):853-861
许文良,王清海,王冬艳,裴福萍,高山.2004.华北克拉通东部中生代岩石圈减薄的过程与机制:中生代火成岩和深源捕虏体证据.地学前缘,11(3):310-317
许文良,杨德彬,裴福萍,于洋.2009.太行山南段符山高镁闪长岩的成因---拆沉陆壳物质熔融的熔体与地幔橄榄岩反应的结果.岩石学报,25(8):1947-1961
杨承海,许文良,杨德彬,王伟,王伟德,刘金民.2008.鲁西上峪辉长-闪长岩的成因:年代学与岩石地球化学证据中国科学(D辑),38(1):44-55
张旗,王焰,李承东,王元龙,金惟俊,贾秀勤.2006.花岗岩的Sr-Yb分类及其地质意义.岩石学报,22(9):2249-2269
张旗,王焰,熊小林,李承东.2008.埃达克岩和花岗岩:挑战和机遇.北京:中国大地出版社,107-129
赵国春,孙敏,Wilde SA.2002.华北克拉通基底构造单元特征及早元古代拼合.中国科学(D辑),32:538-549
赵越,陈斌,张拴宏,刘建民,胡健民,刘健,裴军令.2010.华北克拉通北缘及邻区前燕山期主要地质事件.中国地质,37(4):900-915
郑建平,路凤祥,Reilly SYO,Griffin WL,张明.1999.华北地台东部古生代与新生代岩石圈地幔特征及其演化.地质学报,73(1):47-56
周珣若,吴克隆.1994.漳州I-A型花岗岩.北京:科学出版社,1-152
朱日祥,陈凌,吴福元,刘俊来.2011.华北克拉通破坏的时间、范围与机制.中国科学(地球科学),41(5):583-592
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