宽成分谱系岩墙群的岩石成因及其构造与成矿意义
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摘要
在综述国际上为数不多的宽谱系岩墙群(WSDS)研究实例的基础上,以太行山板内造山带中的岩基后岩墙群为例,详细论证了WSDS的形成机制,并简要讨论其构造与成矿意义。研究认为,1WSDS是一类非常特殊的岩石组合,其岩石组成的多样性主要取决于岩浆起源,因而不同于已知的其他火成岩组合;2WSDS直接的构造指向是造山带岩石圈拆沉作用;3WSDS的产生必须有大规模流体活动的参与,因而是成矿作用的指示器;4岩浆系统是一种复杂性动力系统。在理想系统的框架下,由WSDS识别出的许多成因信息是相矛盾的。但是,在复杂系统的框架下,这些信息可以得到整合解释;5板内造山作用是一种特殊类型的造山作用,与板缘构造力没有直接的联系。WSDS同样适用于板内与板缘2种造山类型,具有普适性,都与岩石圈加厚拆沉有关。
This paper tries to review dike swarms less reported in the world and describe their tectonic and metallogenic implications,defining them as the wide spectrum dike swarms(WSDS). On such a basis, the authors have reached some conclusions:1the WSDS is a specific igneous suite, whose compositional diversity is induced mainly by its origin. Thus the WSDS differs from the other known igneous suites;2the WSDS's direct tectonic meaning is the lithosphere delamination;3Because the producing process of the WSDS needs the active involvement of the deep fluids, the WSDS is the targeting criterion in search for ore deposits;4the magma system is a complex dynamic system. Under the framework of ideal system, many signatures recognized from the WSDS are contradicted. However, these signatures can be integrated under the framework of the complex system;5the intraplate orogen is a specific type of orogen. The orogenesis can not be directly related to the tectonic force from the plate boundaries. WSDS applies equally to intraplate orogen and plate boundary orogen.
This paper tries to review dike swarms less reported in the world and describe their tectonic and metallogenic implications,defining them as the wide spectrum dike swarms(WSDS). On such a basis, the authors have reached some conclusions:1the WSDS is a specific igneous suite, whose compositional diversity is induced mainly by its origin. Thus the WSDS differs from the other known igneous suites;2the WSDS's direct tectonic meaning is the lithosphere delamination;3Because the producing process of the WSDS needs the active involvement of the deep fluids, the WSDS is the targeting criterion in search for ore deposits;4the magma system is a complex dynamic system. Under the framework of ideal system, many signatures recognized from the WSDS are contradicted. However, these signatures can be integrated under the framework of the complex system;5the intraplate orogen is a specific type of orogen. The orogenesis can not be directly related to the tectonic force from the plate boundaries. WSDS applies equally to intraplate orogen and plate boundary orogen.
引文
[1]Scarrow J H,Leat P T,Wareham C D,et al.Geochemistry of mafic dykes in the Antarctic Peninsula continental-margin batholith:a record of arc evolution[J].Contrib.Mineral.Petrol.,1998,131:289-305.
[2]López de Luchi M G,Rapalini A E.Middle Jurassic dyke swarms in the North Patagonian Massif:the Lonco Trapial Formation in the Sierra de Mamil Choique,Río Negro province,Argentina[J].Journal of South American Earth Sciences,2002,15:625-641.
[3]Yang J H,Chung S L,Zhai M G,et al.Geochemical and Sr-NdPb isotopic compositions of mafic dikes from the Jiaodong Peninsula,China:evidence for vein-plus-peridotite melting in the lithospheric mantle[J].Lithos,2004,73:145-160.
[4]罗照华,魏阳,辛厚田,等.造山后脉岩组合的岩石成因——对岩石圈拆沉作用的约束[J].岩石学报,2006,22(6):1672-1684.
[5]El Sayed M M.Geochemistry and petrogenesis of the post-orogenic bimodal dyke swarms in NW Sinai,Egypt:constraints on the magmatic-tectonic processes during the late Precambrian[J].Chemie der Erde,2006,66:129-141.
[6]Féménias O,Berza T,Tatu M,et al.Nature and significance of a Cambro-Ordovician high-K,calc-alkaline sub-volcanic suite:the late-to post-orogenic Motru Dyke Swarm(Southern Carpathians,Romania)[J].International Journal of Earth Sciences,2008,97:479-496.
[7]Allen C M.Evolution of a post-batholith dike swarm in central coastal Queensland,Australia:arc-front to backarc?[J].Lithos,2000,51:331-349.
[8]Tang H F,Zhou X M,Zhi L G.Discovery and significance of Xucun late Proterozoic composite dike swarm in southern Anhui Province[J].Chinese Science Bulletin,1997,42(4):328-330.
[9]Katzir Y,Litvinovsky B A,Jahn B M,et al.Interrelations between coeval mafic and A-type silicic magmas from composite dykes in a bimodal suite of southern Israel,northernmost Arabian-Nubian Shield:Geochemical and isotope constraints[J].Lithos,2007,97:336-364.
[10]罗照华,卢欣祥,王秉璋,等.造山后脉岩组合与内生成矿作用[J].地学前缘,2008,15(4):1-12.
[11]梁涛.安妥岭斑岩型钼矿的成因与深部过程约束[D].北京:中国地质大学(北京)博士学位论文,2010:1-183.
[12]Scarrow J H,Leat P T,Wareham C D,et al.Geochemistry of mafic dykes in the Antarctic Peninsula continental-margin batholith:a record of arc evolution[J].Contrib Mineral Petrol,1998,131:289-305.
[13]Essawy M A,El-Metwally A A.Petrogenesis of a high Ti O2mafic dyke swarm fromsouthwest Sinai[J].Journal of African Earth Sciences,1999,29(3):551-565.
[14]徐义刚,何斌,黄小龙,等.地幔柱大辩论及如何验证地幔柱假说[J].地学前缘,2007,14(2):1-9.
[15]邵济安,张履桥,魏春景.北京南口中生代双峰式岩墙群的组成及其特征[J].岩石学报,2001,75(2):205-212.
[16]邵济安,李献华,张履桥,等.南口—古崖居中生代双峰式岩墙群形成机制的地球化学制约[J].地球化学,2001,30(6):517-524.
[17]邵济安,张履桥.华北北部中生代岩墙群[J].岩石学报,2002,18(3):312-318.
[18]Féménias O,Mercier J C C,Nkono C,et al.Calcic amphibole growth and compositionsin calc-alkaline magmas:evidence from the Motru Dyke Swarm(Southern Carpathians,Romania)[J].American Mineralogist,2006,91:73-81.
[19]Iacumin M,Marzoli A,El-Metwally A A,et al.Neoproterozoic dyke swarms from southern Sinai(Egypt):geochemistry and petrogenetic aspects[J].Journal of African Earth Sciences,1998,26(1):49-64.
[20]罗照华,黄忠敏,柯珊.花岗质岩石的基本问题[J].地质论评,2007,53(增刊):180-226.
[21]Courtillot V,Davaillie A,Besse J,et al.Three distinct types of hotspots in the Earth's mantle[J].Earth and Planetary Science Letters,2003,205:295-308.
[22]Anderson D L.Scoring hotspots:the plume and plate paradigms[C]//Foulger G,Natland J H,Presnall D C,et al.Plates,plumes and paradigms.New York:Geological Society of America,2005,388:31-54.
[23]Petford N.Rheology of granitic magmas during ascent and emplacement[J].Annual Reviews of Earth and Planetary Sciences,2003,31:399-427.
[24]Turner S,Costa F.Measuring Timescales of Magmatic Evolution[J].Elements,2007,3:267-272.
[25]Hart S R,Allégre C J.Trace-element constraints on magma genesis[C]//Hargraves R B.Physics of magmatic processes.New Jersey:Princeton University Press,1980:121-159.
[26]杨宗锋,罗照华,张华锋,等.内蒙古天和永新生代玄武岩成因及其地质意义[J].地学前缘,2009,16(2):90-106.
[27]於崇文.固体地球系统的复杂性与自组织临界性[J].地学前缘,1998,5(3):159-174.
[28]罗照华,莫宣学,万渝生,等.青藏高原最年轻碱性玄武岩SHRIMP年龄的地质意义[J].岩石学报,2006,22(3):578-584.
[29]López de Luchi M G,Rapalini A E.Middle Jurassic dyke swarms in the North Patagonian Massif:the Lonco Trapial Formation in the Sierra de Mamil Choique,Río Negro province.Argentina[J].Journal of South American Earth Sciences,2002,15:625-641.
[30]齐进英.新疆准噶尔脉岩群地质及成因[J].岩石学报,1993,9(3):288-299.
[31]潘颖.北京南口岩墙的岩石学和锆石U-Pb年代学[D].北京:中国地质大学(北京)硕士学位论文,2010:1-68.
[32]罗照华,梁涛,陈必河,等.板内造山作用与成矿[J].岩石学报,2007,23(8):1945-1956.
[33]张旗,金惟俊,李承东,等.中国东部燕山期大规模岩浆活动与岩石圈减薄:与大火成岩省的关系[J].地学前缘,2009,16(2):21-51.
[34]罗照华,魏阳,辛后田,等.太行山中生代板内造山作用与华北大陆岩石圈巨大减薄[J].地学前缘,2006,13(6):52-63.
[35]Koppers A A P,Morgan J P,Morgan J W,et al.Testing the fixed hotspot hypothesis using40Ar/39Ar age progressions along seamount trails[J].Earth and Planetary Science Letters,2001,185:237-252.
[36]罗照华,邓晋福,李玉文等.太行山构造岩浆带K-Ar法同位素年龄分析[J].现代地质,1996,10(3):344-349.
[37]Luo Z H,Deng J F,Cao Y Q,et al.Magmatic activities and orogenic process of Taihangshan intraplate orogen[J].Journal of China University of Geosciences,1999,10(1):76-79.
[38]罗照华,邓晋福,韩秀卿.太行山造山带岩浆活动及其造山过程反演[M].北京:地质出版社,1999:1-124.
[39]覃锋,徐晓霞,罗照华.北京房山岩体形成过程中的岩浆混合作用证据[J].岩石学报,2006,22(12):2957-2970.
[40]Mazzarini F,Corti G,Manetti P,et al.Strain rate and bimodal volcanism in the continental rift:Debre Zeyt volcanic field,northern MER,Ethiopia[J].Journal of African Earth Sciences,2004,39:415-420.
[41]Wilson M.Magmatic differentiation[M].London:Geological Society of London,1993,150:611-624.
[42]Middlemost E A K.Naming materials in the magma/igneous rock system[J].Earth Science Reviews,1994,37(3/4):215-224.
[43]张连昌,万博,焦学军,等.西准包古图含铜斑岩的埃达克岩特征及其地质意义[J].中国地质,2006,33(3):626-631.
[44]Féménias O,Diot H,Berza T,et al.Asymmetrical to symmetrical magnetic fabric of dikes:paleo-flow orientations and paleo-stresses recorded on feeder-bodies from the Motru Dike Swarm(Romania)[J].Journal of Structural Geology,2004,1401-1418.
[45]Nkono C,Féménias O,Diot H,et al.Flowage differentiation in an andesitic dyke of the Motru Dyke Swarm(Southern Carpathians,Romania)inferred from AMS,CSD and geochemistry[J].Journal of Volcanology and Geothermal Research,2006,154:201-221.
[46]White R,Mc Kenzie D.Magmatism at Rift Zones:The Generation of Volcanic Continental Margin sand Flood Basalts[J].Journal of Geophysical Research,1989,94(B6):7685-7729.
[47]Leeman W P,Harry D L.A binary source med el for extension related magmatism in the Great Basin,Western North America[J].Science,1993,262:1550-l554.
[48]Mazzarini F,Corti G,Manetti P,et al.Strain rate and bimodal volcanism in the continental rift:Debre Zeyt volcanic field,northern MER,Ethiopia[J].Journal of African Earth Sciences,2004,39:415-420.
[49]Vigneresse J L,Barbey P,Cuney M.Rheological transitions during partial melting and crystallization with application to felsic magma segregation and transfer[J].Journal of Petrology,1996,37(6):1579-1600.
[50]Petford N.Rheology of granitic magmas during ascent and emplacement[J].Annual Reviews of Earth and Planetary Sciences,2003,31:399-427.
[51]Bachmann O,Bergantz G W.Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies[J].Journal of Volcanology and Geothermal Research,2006,149:85-102.
[52]罗照华,卢欣祥,许俊玉,等.成矿侵入体的岩石学标志[J].岩石学报,2010,26(8):2247-2254.
[53]Gao S,Luo T C,Zhang B R,et al.Chemical composition of the continental crust as revealed by studies in East China[J].Geochimica et Cosmochimica Acta,1998,62(11):1959-1975.
[54]Fan Q C,Liu R X,Li N,et al.Zircon chronologyand REE geochemistry of granulite xenoliths at Hannuoba[J].Chinese Science Bulletin,1998,43:1510-1515.
[55]史兰斌,林传勇,陈孝德,等.由包体推导的河北汉诺坝下地壳—上地幔地温线及其地质意义[J].地震地质,2000,22(1):37-46.
[56]邓晋福,吴宗絮,杨建军,等.格尔木—额济纳旗地学断面走廊域地壳—上地慢岩石学结构与深部过程[J].地球物理学报,1995,38(增刊2):130-144.
[57]Patino Douce A E,Mc Carthy T C.Melting of crustal rocksduring continental collision and subduction[C]//Hacker B R,Liou J G.When continents collide:geodynamics andgeo-chemistry of ultrahigh-pressure rocks.Dordrecht/Boston/London:Kluwer Academic Publishers,1998:27-55.
[58]Patino Douce A E.Vapor-absent melting of tonalite at 15-32k bar[J].Journal of Petrology,2005,46(2):275-290.
[59]Leeman W P,Harry D L.A binary source med el for extension related magmatism in the Great Basin,Western North America[J].Science,1993,262:1550-l554.
[60]Asimow P D,Dixon J E,Lang Tnuir C H.A hydrous melting and fractionation model for mid—ocean ridge basalts:Application to tlle Mid—Atlantic Ridge near the Azores[J].Geochemistry,Geo-physics,Geosystems,2004,5(1):1-24.
[61]樊祺诚,隋建立,刘若新,等.汉诺坝榴辉岩相石榴辉石岩——岩浆底侵作用新证据[J].岩石学报,2001,17(1):1-6.
[62]樊祺诚,隋建立.汉诺坝麻粒岩相-榴辉岩相堆晶岩捕虏体—壳—幔过渡带的证据[J].中国科学基金,2001,15(1):23-27.
[63]Zhou X H,Sun M,Zhang G H,et al.Continental crust and lithospheric mantle interaction beneath North China:isotopic evidence from granulite xenoliths in Hannuoba,Sino-Korean craton[J].Lithos,2002,62:111-124.
[64]Zheng J P,Lu F X,Yu C M,et al.An in situ zircon Hf isotopic,U-Pb age and trace element study of banded granulite xenolith from Hannuoba basalt:Tracking the early evolution of the lower crust in the North China craton[J].Chinese Science Bulletin,2004,49(3):277-285.
[65]邓晋福.大陆裂谷岩浆作用及深部过程[C]//池际尚.中国东部新生代玄武岩及上地幔研究.武汉:中国地质大学出版社,1988:201-218.
[66]邓晋福,赵海玲,罗照华.新生代中国东部大陆岩石圈的伸展与减薄[C]//马杏垣,杨森楠,朱志澄.中国大陆构造论文集.武汉:中国地质大学出版社,1992:165-172.
[67]邓晋福,莫宣学,赵海玲,等.中国东部岩石圈根/去根作用与大陆/活化,东亚型大陆动力学模式研究计划[J].现代地质,1994,8(3):349-356.
[68]Menzies M,Fan W M,Zhang M.Palaeozoic and Cenozoic lithoprobes and the loss of N 120km of Archaean lithosphere,Sino-Korean craton,China[C]//Prichard H M,Alabaster T,Harris N B W,et al.Magmatic Processes and Plate Tectonics.London:Geological Society of London,199,76:71-81.
[69]Deng J F,Mo X X,Zhao H L,et al.A new model for the dynamic evolution of Chinese lithosphere:‘continental roots-plume tectonics’[J].Earth-Science Reviews,2004,65:223-275.
[70]罗照华.吉林辉南大椅山玄武岩中超镁铁岩包体的研究[J].地球科学,1984,(1):73-80.
[71]罗照华,苏尚国,刘翠.大椅山玄武岩中幔源透辉石岩的辉石出溶作用及其地质意义[J].现代地质,2001,15(2):184-188.
[72]Bird P.Initiation of intracontinental subduction in the Himalaya[J].Journal of Geophysical Research,1978,83(B10):4975-4987.
[73]Powell C M,Conagham P J.Plate tectonics and the Himalayas[J].Earth and Planetary Science Letters,1973,20:1-12.
[74]Le Fort P.Himalayas,the collided range-Present knowledge of the continental arc[J].American Journal of Science,1975,175A:1-44.
[75]Hamet J,Allegre C J.Rb-Sr systematics in granite from central Nepal(Manaslu):Significance of the Oligocene age and high87Sr/86Sr ratio in Himalayan orogeny[J].Geology,1976,4:470-472.
[76]Mattauer M.Sur le mécanisme de formation de la schistositédans l’Himalaya[J].Earth and Planetary Science Letters,1975,28:144-154.
[77]Harrison T M,Grove M,Mckeegan K D,et al.Origin and episodic emplacement of the Manaslu intrusive complex,Central Himalaya[J].Journal of Petrology,1999,40(1):3-19.
[78]Searle M P,Godin L.The South Tibetan detachment and the Manaslu leucogranite:A structural reinterpretation and restoration of the Annapurna-Manaslu Himalaya,Nepal[J].The Journal of Geology,2003,111:505-523.
[79]Fyfe W S,Leonardos O H.Ancient metamorphic-migmatite belts of the Brazilian African coasts[J].Nature,1973,244:501-502.
[80]罗照华,柯珊,曹永清,等.东昆仑印支晚期幔源岩浆活动.地质通报,2002,21(6):292-297.
[81]谌宏伟,罗照华,莫宣学,等.东昆仑造山带三叠纪岩浆混合成因花岗岩的岩浆底侵作用机制[J].中国地质,2005,32(3):386-395.
[82]Liu M.Gravitational collapse of mountain belts[c]//Zhang Y X,Yin A.Structure evolution and dynamics of the Earth.Beijing:Higher Education Press,2002:177-205.
[83]Zegers T E,van Keken P E.Middle Archean continent formation by crustal delamination[J].Geology,2001,29(12):1083-1086.
[84]罗照华,辛后田,陈必河,等.壳幔过渡层及其大陆动力学意义[J].现代地质,2007,21(2):421-425.
[85]邓晋福,吴宗絮,赵海玲,等.下地壳性质与壳幔交换[C]//单文琅.岩石圈构造和深部作用.北京:地质出版社,1999:1-7.
[86]Wei W B,Unsworth M,Jones A,et al.Detection of widespread fluids in the Tibetan crust by magnetotelluric studies[J].Science,2001,292:716-718.
[87]Unsworth M J,Jones A G,Wei W B,et al.Crustal rheology of the Himalaya and Southern Tibet inferred from magnetotelluric data[J].Nature,2005,438:78-81.
[88]Wei W B,Ye G F,Jin S,et al.Geoelectric structure of the lithosphere beneath Eastern North China:features of a thinned lithosphere from magnetotelluric soundings[J].Earth Science Frontiers,2008,15(4):204-216.
[89]Nover G.Electrical properties of crustal and mantlerocks—A review of laboratory measurements and their explanation[J].Surveys in Geophysics,2005,26:593-651.
[90]Glover P W J.Graphite and electrical conductivity in the lower continental crust:A review[J].Physics and Chemistry of the Earth,1997,21(4):279-287.
[91]罗照华,卢欣祥,陈必河,等.透岩浆流体成矿作用导论[M].北京:地质出版社,2009:1-177.
[92]Langmuir C H,Klein E M,Plank T.Petrological systematics of mid-ocean ridge basalts:constraints on melt generation beneath ocean ridges[C]//Morgan J P,Blackman D K,Sinton J M.Mantle flow and melt generation at mid-ocean ridges.AGU Geophys Monogr,1992,71:183-280.
[93]石准立,刘凤山.北太行山—燕山区中生代金属矿床成矿系统[J].地学前缘,1999,6(2):297-304.
[94]Caón-Tapia E.How deep can be a dyke?[J].Journal of Volcanology and Geothermal Research,2008,171:215-228.
[95]Brown M,Rushmer T.Evolution and differentiation of the continental crust[M].Cambridge:Cambridge University Press,2006:553.
[96]万天丰,王亚妹,刘俊来.中国东部燕山期和四川期岩石圈构造滑脱与岩浆起源深度[J].地学前缘,2008,15(3):1-35.
[97]罗照华,卢欣祥,陈必河,等.碰撞造山带斑岩型矿床的深部约束机制[J].岩石学报,2008,24(3):447-456.
[98]Li S L,Mooney W D,Fan J C.Crustal structure of mainland China from deep seismic sounding data[J].Tectonophysics,2006,420:239–252.
[99]Zhang Z J,Chen Q F,Bai Z M,et al.Crustal structure and extensional deformation of thinned lithosphere in Northern China[J].Tectonophysics,,2011,508:62-72.
[100]Christensen N I,Mooney W D.Seismic velocity structure andcomposition of the continental crust:a global view[J].Journal of Geophysical Research,1995,100(B5):9761-9788.
[101]Bird P.Continental delamination and the Colorado Plateau[J].Journal of Geophysical Research,1979,84(B13):7561-7571.
[102]Menzies M,Xu Y G,Zhang H F,et al.Integration of geology,geophysics and geochemistry:A key to understanding the North China Craton[J].Lithos,1996:1-21.
[103]Loucks R R,Mavrogenes J A.Gold solubility in supercritical hydrothermal brines measured in synthetic fluid inclusions[J].Science,1999,284:2159-2163.
[104]Korzhinskii D S.Granitization as magmatic replacement[J].Izvestiya Akademii Nauk Kazakhskoi SSR,Seriya Geologicheskaya,1952,2:56-69.
[105]Zotov I A.Transmagmatic magmatizme fluids and ore formation[M].Moscow:Nauka,1989:1-214
[106]黄凡,罗照华,卢欣祥.东沟含钼斑岩由太山庙岩基派生[J].矿床地质,2009,28(5):569-584.
[107]罗照华,莫宣学,卢欣祥,等.透岩浆流体成矿作用—理论分析与野外证据[J].地学前缘,2007,14(3):165-183.
[108]Sparks R S J,Marshall L A.Thermal and mechanical constraints on mixing betweenmafic and silicic magmas[J].Journal of Volcanology and Geothermal Research,1986,29(1):99-124.
[109]李德东,罗照华,周久龙,等.岩墙厚度对成矿作用的约束:以石湖金矿为例[J].地学前缘,2011,18(1):166-178.
[110]Luo Z H,Fan B H,Lu S W,et al.Discovery and metallogenesis of the Antuoling Mo deposit and its implications[J].Northwestern Geology,2009,42(Supp):214-217.
[2]López de Luchi M G,Rapalini A E.Middle Jurassic dyke swarms in the North Patagonian Massif:the Lonco Trapial Formation in the Sierra de Mamil Choique,Río Negro province,Argentina[J].Journal of South American Earth Sciences,2002,15:625-641.
[3]Yang J H,Chung S L,Zhai M G,et al.Geochemical and Sr-NdPb isotopic compositions of mafic dikes from the Jiaodong Peninsula,China:evidence for vein-plus-peridotite melting in the lithospheric mantle[J].Lithos,2004,73:145-160.
[4]罗照华,魏阳,辛厚田,等.造山后脉岩组合的岩石成因——对岩石圈拆沉作用的约束[J].岩石学报,2006,22(6):1672-1684.
[5]El Sayed M M.Geochemistry and petrogenesis of the post-orogenic bimodal dyke swarms in NW Sinai,Egypt:constraints on the magmatic-tectonic processes during the late Precambrian[J].Chemie der Erde,2006,66:129-141.
[6]Féménias O,Berza T,Tatu M,et al.Nature and significance of a Cambro-Ordovician high-K,calc-alkaline sub-volcanic suite:the late-to post-orogenic Motru Dyke Swarm(Southern Carpathians,Romania)[J].International Journal of Earth Sciences,2008,97:479-496.
[7]Allen C M.Evolution of a post-batholith dike swarm in central coastal Queensland,Australia:arc-front to backarc?[J].Lithos,2000,51:331-349.
[8]Tang H F,Zhou X M,Zhi L G.Discovery and significance of Xucun late Proterozoic composite dike swarm in southern Anhui Province[J].Chinese Science Bulletin,1997,42(4):328-330.
[9]Katzir Y,Litvinovsky B A,Jahn B M,et al.Interrelations between coeval mafic and A-type silicic magmas from composite dykes in a bimodal suite of southern Israel,northernmost Arabian-Nubian Shield:Geochemical and isotope constraints[J].Lithos,2007,97:336-364.
[10]罗照华,卢欣祥,王秉璋,等.造山后脉岩组合与内生成矿作用[J].地学前缘,2008,15(4):1-12.
[11]梁涛.安妥岭斑岩型钼矿的成因与深部过程约束[D].北京:中国地质大学(北京)博士学位论文,2010:1-183.
[12]Scarrow J H,Leat P T,Wareham C D,et al.Geochemistry of mafic dykes in the Antarctic Peninsula continental-margin batholith:a record of arc evolution[J].Contrib Mineral Petrol,1998,131:289-305.
[13]Essawy M A,El-Metwally A A.Petrogenesis of a high Ti O2mafic dyke swarm fromsouthwest Sinai[J].Journal of African Earth Sciences,1999,29(3):551-565.
[14]徐义刚,何斌,黄小龙,等.地幔柱大辩论及如何验证地幔柱假说[J].地学前缘,2007,14(2):1-9.
[15]邵济安,张履桥,魏春景.北京南口中生代双峰式岩墙群的组成及其特征[J].岩石学报,2001,75(2):205-212.
[16]邵济安,李献华,张履桥,等.南口—古崖居中生代双峰式岩墙群形成机制的地球化学制约[J].地球化学,2001,30(6):517-524.
[17]邵济安,张履桥.华北北部中生代岩墙群[J].岩石学报,2002,18(3):312-318.
[18]Féménias O,Mercier J C C,Nkono C,et al.Calcic amphibole growth and compositionsin calc-alkaline magmas:evidence from the Motru Dyke Swarm(Southern Carpathians,Romania)[J].American Mineralogist,2006,91:73-81.
[19]Iacumin M,Marzoli A,El-Metwally A A,et al.Neoproterozoic dyke swarms from southern Sinai(Egypt):geochemistry and petrogenetic aspects[J].Journal of African Earth Sciences,1998,26(1):49-64.
[20]罗照华,黄忠敏,柯珊.花岗质岩石的基本问题[J].地质论评,2007,53(增刊):180-226.
[21]Courtillot V,Davaillie A,Besse J,et al.Three distinct types of hotspots in the Earth's mantle[J].Earth and Planetary Science Letters,2003,205:295-308.
[22]Anderson D L.Scoring hotspots:the plume and plate paradigms[C]//Foulger G,Natland J H,Presnall D C,et al.Plates,plumes and paradigms.New York:Geological Society of America,2005,388:31-54.
[23]Petford N.Rheology of granitic magmas during ascent and emplacement[J].Annual Reviews of Earth and Planetary Sciences,2003,31:399-427.
[24]Turner S,Costa F.Measuring Timescales of Magmatic Evolution[J].Elements,2007,3:267-272.
[25]Hart S R,Allégre C J.Trace-element constraints on magma genesis[C]//Hargraves R B.Physics of magmatic processes.New Jersey:Princeton University Press,1980:121-159.
[26]杨宗锋,罗照华,张华锋,等.内蒙古天和永新生代玄武岩成因及其地质意义[J].地学前缘,2009,16(2):90-106.
[27]於崇文.固体地球系统的复杂性与自组织临界性[J].地学前缘,1998,5(3):159-174.
[28]罗照华,莫宣学,万渝生,等.青藏高原最年轻碱性玄武岩SHRIMP年龄的地质意义[J].岩石学报,2006,22(3):578-584.
[29]López de Luchi M G,Rapalini A E.Middle Jurassic dyke swarms in the North Patagonian Massif:the Lonco Trapial Formation in the Sierra de Mamil Choique,Río Negro province.Argentina[J].Journal of South American Earth Sciences,2002,15:625-641.
[30]齐进英.新疆准噶尔脉岩群地质及成因[J].岩石学报,1993,9(3):288-299.
[31]潘颖.北京南口岩墙的岩石学和锆石U-Pb年代学[D].北京:中国地质大学(北京)硕士学位论文,2010:1-68.
[32]罗照华,梁涛,陈必河,等.板内造山作用与成矿[J].岩石学报,2007,23(8):1945-1956.
[33]张旗,金惟俊,李承东,等.中国东部燕山期大规模岩浆活动与岩石圈减薄:与大火成岩省的关系[J].地学前缘,2009,16(2):21-51.
[34]罗照华,魏阳,辛后田,等.太行山中生代板内造山作用与华北大陆岩石圈巨大减薄[J].地学前缘,2006,13(6):52-63.
[35]Koppers A A P,Morgan J P,Morgan J W,et al.Testing the fixed hotspot hypothesis using40Ar/39Ar age progressions along seamount trails[J].Earth and Planetary Science Letters,2001,185:237-252.
[36]罗照华,邓晋福,李玉文等.太行山构造岩浆带K-Ar法同位素年龄分析[J].现代地质,1996,10(3):344-349.
[37]Luo Z H,Deng J F,Cao Y Q,et al.Magmatic activities and orogenic process of Taihangshan intraplate orogen[J].Journal of China University of Geosciences,1999,10(1):76-79.
[38]罗照华,邓晋福,韩秀卿.太行山造山带岩浆活动及其造山过程反演[M].北京:地质出版社,1999:1-124.
[39]覃锋,徐晓霞,罗照华.北京房山岩体形成过程中的岩浆混合作用证据[J].岩石学报,2006,22(12):2957-2970.
[40]Mazzarini F,Corti G,Manetti P,et al.Strain rate and bimodal volcanism in the continental rift:Debre Zeyt volcanic field,northern MER,Ethiopia[J].Journal of African Earth Sciences,2004,39:415-420.
[41]Wilson M.Magmatic differentiation[M].London:Geological Society of London,1993,150:611-624.
[42]Middlemost E A K.Naming materials in the magma/igneous rock system[J].Earth Science Reviews,1994,37(3/4):215-224.
[43]张连昌,万博,焦学军,等.西准包古图含铜斑岩的埃达克岩特征及其地质意义[J].中国地质,2006,33(3):626-631.
[44]Féménias O,Diot H,Berza T,et al.Asymmetrical to symmetrical magnetic fabric of dikes:paleo-flow orientations and paleo-stresses recorded on feeder-bodies from the Motru Dike Swarm(Romania)[J].Journal of Structural Geology,2004,1401-1418.
[45]Nkono C,Féménias O,Diot H,et al.Flowage differentiation in an andesitic dyke of the Motru Dyke Swarm(Southern Carpathians,Romania)inferred from AMS,CSD and geochemistry[J].Journal of Volcanology and Geothermal Research,2006,154:201-221.
[46]White R,Mc Kenzie D.Magmatism at Rift Zones:The Generation of Volcanic Continental Margin sand Flood Basalts[J].Journal of Geophysical Research,1989,94(B6):7685-7729.
[47]Leeman W P,Harry D L.A binary source med el for extension related magmatism in the Great Basin,Western North America[J].Science,1993,262:1550-l554.
[48]Mazzarini F,Corti G,Manetti P,et al.Strain rate and bimodal volcanism in the continental rift:Debre Zeyt volcanic field,northern MER,Ethiopia[J].Journal of African Earth Sciences,2004,39:415-420.
[49]Vigneresse J L,Barbey P,Cuney M.Rheological transitions during partial melting and crystallization with application to felsic magma segregation and transfer[J].Journal of Petrology,1996,37(6):1579-1600.
[50]Petford N.Rheology of granitic magmas during ascent and emplacement[J].Annual Reviews of Earth and Planetary Sciences,2003,31:399-427.
[51]Bachmann O,Bergantz G W.Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies[J].Journal of Volcanology and Geothermal Research,2006,149:85-102.
[52]罗照华,卢欣祥,许俊玉,等.成矿侵入体的岩石学标志[J].岩石学报,2010,26(8):2247-2254.
[53]Gao S,Luo T C,Zhang B R,et al.Chemical composition of the continental crust as revealed by studies in East China[J].Geochimica et Cosmochimica Acta,1998,62(11):1959-1975.
[54]Fan Q C,Liu R X,Li N,et al.Zircon chronologyand REE geochemistry of granulite xenoliths at Hannuoba[J].Chinese Science Bulletin,1998,43:1510-1515.
[55]史兰斌,林传勇,陈孝德,等.由包体推导的河北汉诺坝下地壳—上地幔地温线及其地质意义[J].地震地质,2000,22(1):37-46.
[56]邓晋福,吴宗絮,杨建军,等.格尔木—额济纳旗地学断面走廊域地壳—上地慢岩石学结构与深部过程[J].地球物理学报,1995,38(增刊2):130-144.
[57]Patino Douce A E,Mc Carthy T C.Melting of crustal rocksduring continental collision and subduction[C]//Hacker B R,Liou J G.When continents collide:geodynamics andgeo-chemistry of ultrahigh-pressure rocks.Dordrecht/Boston/London:Kluwer Academic Publishers,1998:27-55.
[58]Patino Douce A E.Vapor-absent melting of tonalite at 15-32k bar[J].Journal of Petrology,2005,46(2):275-290.
[59]Leeman W P,Harry D L.A binary source med el for extension related magmatism in the Great Basin,Western North America[J].Science,1993,262:1550-l554.
[60]Asimow P D,Dixon J E,Lang Tnuir C H.A hydrous melting and fractionation model for mid—ocean ridge basalts:Application to tlle Mid—Atlantic Ridge near the Azores[J].Geochemistry,Geo-physics,Geosystems,2004,5(1):1-24.
[61]樊祺诚,隋建立,刘若新,等.汉诺坝榴辉岩相石榴辉石岩——岩浆底侵作用新证据[J].岩石学报,2001,17(1):1-6.
[62]樊祺诚,隋建立.汉诺坝麻粒岩相-榴辉岩相堆晶岩捕虏体—壳—幔过渡带的证据[J].中国科学基金,2001,15(1):23-27.
[63]Zhou X H,Sun M,Zhang G H,et al.Continental crust and lithospheric mantle interaction beneath North China:isotopic evidence from granulite xenoliths in Hannuoba,Sino-Korean craton[J].Lithos,2002,62:111-124.
[64]Zheng J P,Lu F X,Yu C M,et al.An in situ zircon Hf isotopic,U-Pb age and trace element study of banded granulite xenolith from Hannuoba basalt:Tracking the early evolution of the lower crust in the North China craton[J].Chinese Science Bulletin,2004,49(3):277-285.
[65]邓晋福.大陆裂谷岩浆作用及深部过程[C]//池际尚.中国东部新生代玄武岩及上地幔研究.武汉:中国地质大学出版社,1988:201-218.
[66]邓晋福,赵海玲,罗照华.新生代中国东部大陆岩石圈的伸展与减薄[C]//马杏垣,杨森楠,朱志澄.中国大陆构造论文集.武汉:中国地质大学出版社,1992:165-172.
[67]邓晋福,莫宣学,赵海玲,等.中国东部岩石圈根/去根作用与大陆/活化,东亚型大陆动力学模式研究计划[J].现代地质,1994,8(3):349-356.
[68]Menzies M,Fan W M,Zhang M.Palaeozoic and Cenozoic lithoprobes and the loss of N 120km of Archaean lithosphere,Sino-Korean craton,China[C]//Prichard H M,Alabaster T,Harris N B W,et al.Magmatic Processes and Plate Tectonics.London:Geological Society of London,199,76:71-81.
[69]Deng J F,Mo X X,Zhao H L,et al.A new model for the dynamic evolution of Chinese lithosphere:‘continental roots-plume tectonics’[J].Earth-Science Reviews,2004,65:223-275.
[70]罗照华.吉林辉南大椅山玄武岩中超镁铁岩包体的研究[J].地球科学,1984,(1):73-80.
[71]罗照华,苏尚国,刘翠.大椅山玄武岩中幔源透辉石岩的辉石出溶作用及其地质意义[J].现代地质,2001,15(2):184-188.
[72]Bird P.Initiation of intracontinental subduction in the Himalaya[J].Journal of Geophysical Research,1978,83(B10):4975-4987.
[73]Powell C M,Conagham P J.Plate tectonics and the Himalayas[J].Earth and Planetary Science Letters,1973,20:1-12.
[74]Le Fort P.Himalayas,the collided range-Present knowledge of the continental arc[J].American Journal of Science,1975,175A:1-44.
[75]Hamet J,Allegre C J.Rb-Sr systematics in granite from central Nepal(Manaslu):Significance of the Oligocene age and high87Sr/86Sr ratio in Himalayan orogeny[J].Geology,1976,4:470-472.
[76]Mattauer M.Sur le mécanisme de formation de la schistositédans l’Himalaya[J].Earth and Planetary Science Letters,1975,28:144-154.
[77]Harrison T M,Grove M,Mckeegan K D,et al.Origin and episodic emplacement of the Manaslu intrusive complex,Central Himalaya[J].Journal of Petrology,1999,40(1):3-19.
[78]Searle M P,Godin L.The South Tibetan detachment and the Manaslu leucogranite:A structural reinterpretation and restoration of the Annapurna-Manaslu Himalaya,Nepal[J].The Journal of Geology,2003,111:505-523.
[79]Fyfe W S,Leonardos O H.Ancient metamorphic-migmatite belts of the Brazilian African coasts[J].Nature,1973,244:501-502.
[80]罗照华,柯珊,曹永清,等.东昆仑印支晚期幔源岩浆活动.地质通报,2002,21(6):292-297.
[81]谌宏伟,罗照华,莫宣学,等.东昆仑造山带三叠纪岩浆混合成因花岗岩的岩浆底侵作用机制[J].中国地质,2005,32(3):386-395.
[82]Liu M.Gravitational collapse of mountain belts[c]//Zhang Y X,Yin A.Structure evolution and dynamics of the Earth.Beijing:Higher Education Press,2002:177-205.
[83]Zegers T E,van Keken P E.Middle Archean continent formation by crustal delamination[J].Geology,2001,29(12):1083-1086.
[84]罗照华,辛后田,陈必河,等.壳幔过渡层及其大陆动力学意义[J].现代地质,2007,21(2):421-425.
[85]邓晋福,吴宗絮,赵海玲,等.下地壳性质与壳幔交换[C]//单文琅.岩石圈构造和深部作用.北京:地质出版社,1999:1-7.
[86]Wei W B,Unsworth M,Jones A,et al.Detection of widespread fluids in the Tibetan crust by magnetotelluric studies[J].Science,2001,292:716-718.
[87]Unsworth M J,Jones A G,Wei W B,et al.Crustal rheology of the Himalaya and Southern Tibet inferred from magnetotelluric data[J].Nature,2005,438:78-81.
[88]Wei W B,Ye G F,Jin S,et al.Geoelectric structure of the lithosphere beneath Eastern North China:features of a thinned lithosphere from magnetotelluric soundings[J].Earth Science Frontiers,2008,15(4):204-216.
[89]Nover G.Electrical properties of crustal and mantlerocks—A review of laboratory measurements and their explanation[J].Surveys in Geophysics,2005,26:593-651.
[90]Glover P W J.Graphite and electrical conductivity in the lower continental crust:A review[J].Physics and Chemistry of the Earth,1997,21(4):279-287.
[91]罗照华,卢欣祥,陈必河,等.透岩浆流体成矿作用导论[M].北京:地质出版社,2009:1-177.
[92]Langmuir C H,Klein E M,Plank T.Petrological systematics of mid-ocean ridge basalts:constraints on melt generation beneath ocean ridges[C]//Morgan J P,Blackman D K,Sinton J M.Mantle flow and melt generation at mid-ocean ridges.AGU Geophys Monogr,1992,71:183-280.
[93]石准立,刘凤山.北太行山—燕山区中生代金属矿床成矿系统[J].地学前缘,1999,6(2):297-304.
[94]Caón-Tapia E.How deep can be a dyke?[J].Journal of Volcanology and Geothermal Research,2008,171:215-228.
[95]Brown M,Rushmer T.Evolution and differentiation of the continental crust[M].Cambridge:Cambridge University Press,2006:553.
[96]万天丰,王亚妹,刘俊来.中国东部燕山期和四川期岩石圈构造滑脱与岩浆起源深度[J].地学前缘,2008,15(3):1-35.
[97]罗照华,卢欣祥,陈必河,等.碰撞造山带斑岩型矿床的深部约束机制[J].岩石学报,2008,24(3):447-456.
[98]Li S L,Mooney W D,Fan J C.Crustal structure of mainland China from deep seismic sounding data[J].Tectonophysics,2006,420:239–252.
[99]Zhang Z J,Chen Q F,Bai Z M,et al.Crustal structure and extensional deformation of thinned lithosphere in Northern China[J].Tectonophysics,,2011,508:62-72.
[100]Christensen N I,Mooney W D.Seismic velocity structure andcomposition of the continental crust:a global view[J].Journal of Geophysical Research,1995,100(B5):9761-9788.
[101]Bird P.Continental delamination and the Colorado Plateau[J].Journal of Geophysical Research,1979,84(B13):7561-7571.
[102]Menzies M,Xu Y G,Zhang H F,et al.Integration of geology,geophysics and geochemistry:A key to understanding the North China Craton[J].Lithos,1996:1-21.
[103]Loucks R R,Mavrogenes J A.Gold solubility in supercritical hydrothermal brines measured in synthetic fluid inclusions[J].Science,1999,284:2159-2163.
[104]Korzhinskii D S.Granitization as magmatic replacement[J].Izvestiya Akademii Nauk Kazakhskoi SSR,Seriya Geologicheskaya,1952,2:56-69.
[105]Zotov I A.Transmagmatic magmatizme fluids and ore formation[M].Moscow:Nauka,1989:1-214
[106]黄凡,罗照华,卢欣祥.东沟含钼斑岩由太山庙岩基派生[J].矿床地质,2009,28(5):569-584.
[107]罗照华,莫宣学,卢欣祥,等.透岩浆流体成矿作用—理论分析与野外证据[J].地学前缘,2007,14(3):165-183.
[108]Sparks R S J,Marshall L A.Thermal and mechanical constraints on mixing betweenmafic and silicic magmas[J].Journal of Volcanology and Geothermal Research,1986,29(1):99-124.
[109]李德东,罗照华,周久龙,等.岩墙厚度对成矿作用的约束:以石湖金矿为例[J].地学前缘,2011,18(1):166-178.
[110]Luo Z H,Fan B H,Lu S W,et al.Discovery and metallogenesis of the Antuoling Mo deposit and its implications[J].Northwestern Geology,2009,42(Supp):214-217.