河北小寺沟铜钼矿埃达克岩:年龄、地球化学特征及其地质意义
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摘要
小寺沟斑岩型铜钼矿产于华北板块北缘,其主体岩体类型为英云闪长岩和二长花岗岩类,矿物组合为斜长石+角闪石+石英+钾长石±黑云母±辉石+不透明矿物,岩性为钙碱性I型侵入岩。K-Ar法测得小寺沟岩体花岗斑岩年龄为(122.83±2.46)Ma。岩石主量元素具有高SiO2、Al2O3、Na2O、Mg#,低K2O、TiO2、MgO、CaO、P2O5特征。稀土元素具有负Eu异常不明显,低HREE和Y,轻、重稀土元素强烈分异特征。研究认为,小寺沟岩体与埃达克岩相似,其初始岩浆主要为加厚下地壳的部分熔融产物,即小寺沟埃达克岩为C型埃达克岩,其初始岩浆中可能还有部分地幔物质。小寺沟大型斑岩型铜钼矿的形成与埃达克岩的成矿专属性、华北板块北缘特殊构造环境密切相关。
The Xiaosigou porphyry deposit occurs in the northern margin of North China craton,which belongs to the East Circum-Pacific metallogenic domain.The Xiaosigou pluton is comprised of tonalite and monzonitic granite,which are both I-type granites,with the mineral assemblage being plagioclase+ amphibole+ quartz+ potassium feldspar±biotite±pyroxene+some opaque minerals.K-Ar dating of unaltered granite-porphyry yielded an age of(122.83±2.46) Ma.SiO2,Al2O3, Na2O and Mg# are high whereas K2O,TiO2,MgO,CaO and P2O5 are relatively low.The Xiaosigou pluton is characterized by slightly negative to positive δEu anomalies,the lowness of HREE and Y,and the intense fractionation of LREE from HREE.These characteristics suggest that the Xiaosigou pluton is extremely similar to adakite.The primitive magma of the Xiaosigou pluton was derived from the partially melted lower crust as well as some mantle materials.The Xiaosigou large-size porphyry copper-molybdenum deposit is genetically in close connection with adakite and the tectonic environment of the northern edge of North China craton.
The Xiaosigou porphyry deposit occurs in the northern margin of North China craton,which belongs to the East Circum-Pacific metallogenic domain.The Xiaosigou pluton is comprised of tonalite and monzonitic granite,which are both I-type granites,with the mineral assemblage being plagioclase+ amphibole+ quartz+ potassium feldspar±biotite±pyroxene+some opaque minerals.K-Ar dating of unaltered granite-porphyry yielded an age of(122.83±2.46) Ma.SiO2,Al2O3, Na2O and Mg# are high whereas K2O,TiO2,MgO,CaO and P2O5 are relatively low.The Xiaosigou pluton is characterized by slightly negative to positive δEu anomalies,the lowness of HREE and Y,and the intense fractionation of LREE from HREE.These characteristics suggest that the Xiaosigou pluton is extremely similar to adakite.The primitive magma of the Xiaosigou pluton was derived from the partially melted lower crust as well as some mantle materials.The Xiaosigou large-size porphyry copper-molybdenum deposit is genetically in close connection with adakite and the tectonic environment of the northern edge of North China craton.
引文
Atherton MP and Petford N.1993.Generation of sodium-rich magmasfromnewly underplated basaltic crust[J].Nature,362:144-146.
Batchlo R Aand Bowden P.1985.Petrogeneticinterpretationof granotoidrock series using multination parameters[J].Chem.Goel.,48(1/4):43-55.
Bo T B and Zhao B.1990.Geological and geochemical evidence of con-temporaneity and consanguinity of the Xiaosigou porphyry depositand its coexisting skarn deposits[J].Geochemical,2:166-174(in Chinese with English abstract).
Chappell B Wand White AJ R.1974.Two contrasting granitetype[J].Pacific Geology,173-174.
Chung S L,Liu D Y,Ji J Q,Chu MF,Lee H Y,Wen D J,Lo C H,Lee T Y,Qian Qand Zhang Q.2003.Adakites fromcontinentalcollision zone:Melting of thickened lower-crust beneath southeastTibet[J].Geology,31(11):1021-1024.
Defant MJ and Drummond MS.1990.Derivation of some modern arcmagmas by melting of young subduction lithosphere[J].Nature,347:662-665.
Defant MJ,Richerson M,De Boer J Z,Stewart R H,Maury R C,Bellon H,Drummond M S,Feigenson M D and Jackson T E.1991.Dacite genesis via both slab melting and differentiation:Pet-rogenesis of La Yeguada volcanic complex[J].Panama J.Petrol.,32:1101-1142.
Defant MJ and Drummond MS.1993.Mount St Helens:Potential ex-ample of the partial melting of the subductedlithospherein a volcanicarc[J].Geology,21:547-550.
DengJ F,Zhao HL,Mo X Xand Luo Z H.1996.The key of continen-tal root-pole tectonics and the dynamics in china[M].Beijing:Geol.Pub.House.1-110(in Chinese).
Deng J F,Zhao G C,Zhao J L,Luo Z H,Dai S Qand Li K M.2000.Yanshanian igneous petrotectonic assemblages and orogenic-deepprocessesin east China[J].Geological Review,46(1):41-48(inChinese with English abstract).
Dong S W,Wu X H,Wu Z H,Deng J F,Gao Yand Wang C S.2000.Ontectonic seesawing of the east Asia continent-global i mplication ofthe Yanshanian movement[J].Geological Review,46(1):8-13(inChinese with English abstract).
Drummond M S and Defant M J.1990.A model for trondhjemite-tonalite adakitic genesis and crustal growth via slab melting:Ar-chaean to modern comparisons[J].Geophys.Res.,95:21503-21521.
Fang WX,Yang S F,Liu Z T,Wei X L and Zhang B C.2007.Geo-chemical characteristics and significance of major element,trace ele-ments and REEin mineralized altered rocks of large scale TsagaanSuvarga Cu-Mo porphyry deposit in Mongolia[J].Journal of theChinese Rare Earth Society,25(1),85-94(in Chinese with Eng-lish abstract).
Gao B S and Zheng Y Y.2006.Geochemical controlling of mineraliza-tionin Qulong super-large porphyry copper deposit,Tibet[J].Geo-logical Science and Technology Information,25(2):41-46(in Chi-nese with English abstract).
Gregory A Davis.2003.The Yanshanian belt of north China:Tectonics,adakitic magmatism,and crustal evolution[J].Earth Science Fron-tiers,12(4):373-384.
Han X Land Yin LJ.1999.The study onthe ore-controlledfactors andmetallogenic regularity of Xiaosigou Cu-Mo deposit[J].Journal ofHebei Institute of Technology,21(2):62-66(in Chinese withEnglish abstract).
Hollister V F and Sirvas E B.1974.The Michiquillay porphyry copperdeposit[J].Mineraium Deposita,9(2):261-269.
Hollings P and Kerrich R.2000.An Archean arc basalt-Nb-enrichedbasalt-adakite association:The2.7Ga confederation assemblages ofthe Birch-Uchi greenstone belt,Superior Province[J].Contrions toMineralogy and Petrology,139:208-226.
Hou Z Q,Mo X X,Gao Y F,Qu X Mand Meng XJ.2003.Adakite,Apossible host rock for porphyry copper deposits:Case studies ofporphyry copper belts in Tibetan plateau and in northern Chile[J].Mineral Deposits,22(1):1-12(in Chinese with English abstract).
Hu XZ.1988.Discussion of characteristics and genesisin Yeji wei quartzporphyry rocks with tin[A].In:Huxiang Zhao Technology[C].Changsha:Central South University Press.24-30(in Chinese withEnglish abstract).
Isbibara S.1977.The magnetite-series andil menite-series granitic rocks[J].Mining Geology,27:293-305.
Kepezhinskas P K,Defant MJ and Drummond MS.1996.Progressiveenrichment of island arc mantle by melt-peridotite interaction in-ferred from Kamchatka xenoliths[J].Geochi m.Cosmochi m.Acta,60:1217-1229.
Li WC and Zeng P S.2007.Characteristics and metallogenic model ofthe Pulang super-large porphyry copper deposit in Yunnan,China[J].Journal of Chengdu University of Technology,34(4):436-446(in Chinese with English abstract).
Marc J D,Xu J F,Pavel K,Wang Q,Zhang Q and Xiao L.2002.Adakites:Some variations on a theme[J].Acta Petrologica Sinica,18(2):129-142.
Martin H.1999.Adakitic magmas:Modern analogues of Archaeangranitoids[J].Lithos,46:411-429.
Morris P A.1995.Slab melting as an explanation of Quaternary volcan-ismand aseismicity in southwestern Japan[J].Geology,23:395-398.
Nelson K D.1992.Are crustal thickness variations in old mountain beltlike the Appalachians a consequence of lithospheres delaminating[J]?Geology,20(06):498-502.
Patino Douce A E.1997.Generation of metal minerals:A-type granitesbylowpressure melting of calc-alkaline granitites[J].Geology,25(02):743-746.
Peacock S M,Rushmer Tand Thompson AB.1994.Partial melting ofsubducting oceanic crust[J].Earth Planet Sci.Lett.,121:227-244.
Peacock S Mand Wang K.1999.Seismic consequences of warmversuscool subduction metamorphism:Examples from southwest andnortheast Japan[J].Sciences,286:937-939.
Philip R Wand James F L.1998.Rare earth element metasomatisminhydrothermal systerms:The Willsboro-Lewis wollastonite ores,New York,USA[J].Geochem.Cosmochi m.Acta,62(17):2964-2968.
Qin J F,Lai S C and Li Y F.2007.Genesis of the Indosinian Guang-toushan adakitic biotite plagiogranite in the Mianxian-Lueyang(Mi-anlue)suture,south Qingling,and its tectonic i mplications[J].Geological Bulletin of China,26(4):466-471(in Chinese with Eng-lish abstract).
Rapp R P,Watson E Band Miller C F.1991.Partial melting of amphi-bolites ecologies and the origin of Achaean trend emits and tonalities[J].Precambrian Research,51(05):1-25.
Rapp R P and Watson E B.1995.Dehydration melting of metabasalt at8-32Kbar:I mplications for continental growth and crust-mantle re-cycling[J].Petrol.,36:891-931.
Rapp R P,Shi mizu Nand Norman MD.1999.Reaction between slab-derived melts and peridotiteinthe mantle wedge:Experi mental con-straints at3.8Gpa[J].Chemical Geology,160:335-356.
Rapp R P,Xiao L and Shi mizu N.2002.Experi mental constraints onthe origin of potassium-rich adakites in eastern China[J].ActaPetrologica Sinica,18(3):293-302.
Ren J S.1999.Tectonic map of China and adjacent region[M].Beijing:Geol.Pub.House.1-50(in Chinese).
Rui Z Y,Hang C K and Qi M G.1984.Porphyry copper(molybde-num)in China[M].Beijing:Geol.Pub.House.1-350(in Chi-nese).
Sen C and Dunn T.1994.Dehydration melting of a basaltic compositionamphibolite at1.5and2.0GPa:I mplications for the origin ofadakites[J].Contrib.Miner.Petrol.,117:394-409.
Sillitoe R H.1972.A plate tectonic model for the origin of porphyrycopper deposits[J].Econ.Geol.,67:184-197.
Springer Wand Seck HA.1997.Partial fusion of basic granulites at5to15Kbar:I mplications for the origin of TTG magmas[J].Contrib.Miner.Petrol.,127:30-45.
Stern C Rand Kilian R.1996.Role of the subductedslab,mantle wedgeand continental crust in the generation of adakites fromthe Australvolcanic zone[J].Contrib.Miner.Petrol.,123:263-281.
Sun J F,Wang H Wand Xu Z H.2004.Study on the Ag mineral re-source potential in the surrounding of Xiaosigou Cu-Mo deposit inthe north Hebei Province[J].Contributions to Geology and MineralResources Research,9(1):20-23(in Chinese with English ab-stract).
Sylverster P J.1998.Post-collision strongly peraluminous granites[J].Lithos,45:29-44.
Thieblemont D and Lehrberger J L.1997.Gisements epithermal andporphyry:A connection adakite[J].Earth Planet.Sci.Lett.,325:103-109.
Tu G Z.1989.Prospecting and theory about super-large deposits[J].Advancein Earth Sciences,6:14-20(in Chinese with English ab-stract).
Wang Q,Xu J F,Wang J X,Zhao Z H,Wang RJ,Qiu J X,Xiong XL,Sang L Kand Peng L H.2000.The recognition of adakite-typegneissesin the north Dabie Mountains and the relationship betweenthemand ultrahigh pressure metamorphism[J].Chinese ScienceBulletin,46(10):1017-1024(in Chinese).
Wang Q,Zhao Z H,Xiong X L and Xu J F.2001.Melting of the un-derplated basalticlower crust:Evidence fromthe Shaxi adakitic sod-ic quartz diorite-porphyrites,Anhui Province,China[J].Geochi mi-ca,30(4):353-362(in Chinese with English abstract).
Wang Q,Zhao Z H,Xu J F,Bai Z H,Wang J Xand Liu C X.2004.The geochemical comparison between the Tongshankou and Yinzuadakitic intrusive rocksin southeastern Hubei:(Delaminated)Low-er crustal melting and the genesis of porphyry copper deposit[J].Acta Petrologica Sinica,20(2):351-360(in Chinese with Englishabstract).
Wang Y,Zhang Qand Qian Q.2000.Adakite geochemical characteris-tics andtectonic significances[J].Scientia Geologica Sinica,35(2):251-256(in Chinese with English abstract).
Wang Y L,Zhang Q,Wang Q,Liu HTand Wang Y.2003.Study onadakitic rock and Cu-Au mineralization[J].Acta Petrologica Sinica,19(3):543-550(in Chinese with English abstract).
Wang Y L,Wang Y,Zhang Q,Jia X Qand Han S.2004.The geo-chemical characteristics of Mesozoic intermediate-acid intrusives ofthe Tongling area and its metallogenesis geodynamic i mplications[J].Acta Petrologica Sinica,20(2):325-338(in Chinese withEnglish abstract).
Xiao Q H,Deng F Q,Ma D S,Hong D Wand Mo X X.2002.Thethought and meanings in the granites research[M].Beijing:Geol.Pub.House.12-63(in Chinese).
Xie Q Q,Xu X C,Li X X,Cheng T Hand Lu S M.2006.Rare earthelements geochemistry of Laowan gold deposit in Henan Province:Trace to source of ore-forming materials[J].Journal of RareEarths,24(1):114-119
Xu J F,Shinjo R,Defant MJ and Wang Q.2002.Origin of Mesozoicadakitic intrusive rocks in the Ningzhen area of east China:Partialmelting of delaminated lower continental crust[J]?Geology,30:1111-1114.
Xu L Q,Deng J F,Chen Z Yand Tao J X.2003.Theidentification ofOrdovician adakites and its signification in northern Damao,innerMongolia[J].Geoscience,17(4):428-434(in Chinese with Eng-lish abstract).
Yin B C and Yan Q C.1997.The tectonic environments of metalloge-niesis of Duobaoshan super-large copper deposit[J].Acta Miner-alogica Sinica,17(2):220-224(in Chinese with English abstract).
Yogodzinski G M,Kay R W,Volynets O N,Kay S Mand Koloskov AV.1995.Magnesian andesiteinthe western Aleutian Komandorskyregion:I mplications for slab melting and processes in the mantlewedge[J].Geol.Society Am.Bull.,107:505-519.
Yu L F,Yang X Y,Sun WD,Chi Y Yand Zhang Q M.2008.Theadakite and mineralization of the Shaxi porphyry copper-gold de-posit,central Anhui[J].Geologyin China,35(6):1150-1161(inChinese with English abstract).
Zhai YS,Zhang Hand SongJ L.1997.Largetectonics andsuper-largedeposits[M].Beijing:Geol.Pub.House.152-169(in Chinese).
Zhang HT,Chen R Yand Han F L.2004.Re-understanding of metal-logenic geological conditions of porphyry copper deposits in China[J].Mineral Deposits,23(2):150-163(in Chinese with Englishabstract).
Zhang Q,Qian Q,Wang E C,Wang Y,Zaho TP,Hao J and Guo GJ.2001a.An east China plateauin mid-late Yanshanian period:I mpli-cation fromadakites[J].Chinese Journal of Geology,36(2):248-255(in Chinese with English abstract).
Zhang Q,Wang Y and Wang Y L.2001b.Preli minary study on thecomponents of the lower crust in east China Plateau during Yan-shani-an period:Constraints on Sr and Ndisotopic compositions ofadaklte-like rocks[J].Acta Petrologica Sinica,17(4):505-513(inChinese with English abstract).
Zhang Q,Wang Y,Liu H T,Wang Y L and Li Z T.2003a.On thespaceti me distribution and geodynamic environments of adakites inChina annex:Controversies over differing opinions for adakites inChina[J].Earth Science Frontiers,10(4):385-400(in Chinesewith English abstract).
Zhang Q,Wang Yand Wang Y L.2003b.Onthe relationship betweenAdakite andits tectonic setting[J].Geotectonica et Metallogenia,27(02):101-108(in Chinese with English abstract).
Zhang Q,Xu J F,Wang Y,Xiao L,Liu H T and Wang Y L.2004.Diversity of adakite[J].Geological Bulletin of China,23(9/l0):959-965(in Chinese with English abstract).
Zhang Q,Jin WJ,Wang Y L,Li C D,Wang Yand Jia X Q.2006.Ocean lithosphere delamination and the lower crust delamination:The different mechanism and geological i mplication:Comment onthe delamination model of lower crust and lithosphere mantle[J].Acta Petrologica Sinica,22(11):2631-2638(in Chinese with Eng-lish abstract).
Zhang Q.2008.Adakite research:Retrospect and prospect[J].Geologyin China,35(1):32-39(in Chinese with English abstract).
Zhao WJ.2007.Deep tectono-magmatic setting for metallogenesis oflarge porphyry copper deposits[J].Geologyin China,34(2):179-205(in Chinese with English abstract).
Zhou G,Zhang Z C,Luo S B,He B,Wang X,Ying LJ,Zhao H,Li AHand He Y K.2007.Confirmation of high-temperature stronglyperaluminous Mayin’ebo granitesinthe south margin of Altay,Xin-jiang:Age,geochemistry and tectonic i mplications[J].Acta Petro-logica Sinica,23(8):1909-1020(in Chinese with English ab-stract).
柏天宝,赵斌.1990.小寺沟斑岩矿床及其共生的矽卡岩矿床的周期性、同源性的地质地球化学证据[J].地球化学,(2):166-174.
邓晋福,赵海玲,莫宣学,罗照华.1996.中国大陆根-柱构造-大陆动力学的钥匙[M].北京:地质出版社.1-110.
邓晋福,赵国春,赵海玲,罗照华,戴圣潜,李凯明.2000.中国东部燕山期火成岩构造组合与造山深部过程[J].地质论评,46:41-48.
董树文,吴锡浩,吴珍汉,邓晋福,高锐,王成善.2000.论东亚大陆的构造翘变———燕山运动的全球意义[J].地质论评,46:8-13.
方维萱,杨杜锋,刘正桃,韦星林,张宝琛.2007.蒙古查干苏布尔加(Tsagaan Suvarga)大型斑岩型铜钼矿床含矿蚀变岩常量、微量和稀土元素地球化学特征及意义[J].中国稀土学报,25(1):85-94.
高宝顺,郑有业.2006.西藏驱龙超大型斑岩铜矿床成矿作用的地球化学控制[J].地质科技情报,25(2):41-46.
韩秀丽,尹力军.1999.小寺沟铜钼矿床控矿因素及成矿规律[J].河北理工学院学报,21(2):62-66.
候增谦,莫宣学,高永丰,曲晓明,孟祥金.2003.埃达克岩:斑岩铜矿的一种可能的重要含矿母岩[J].矿床地质,22(1):1-12.
胡祥昭.1988.野鸡尾含锡石英斑岩的岩石学特征及成因探讨[A].胡祥昭论文集[C].长沙:中南大学出版社.24-30.
李文昌,曾普胜.2007.云南普朗超大型斑岩铜矿特征及成矿模型[J].成都理工大学学报,34(4):436-446.
秦江峰,赖绍聪,李永飞.2007.南秦岭勉县-略阳缝合带印支期光头山埃达克质花岗岩的成因及其地质意义[J].地质通报,26(4):466-471.
任纪舜.1999.中国及邻区大地构造图[M].北京:地质出版社.1-50.
芮宗瑶,黄崇轲,齐国明.1984.中国斑岩铜(钼)矿床[M].北京:地质出版社.1-350.
孙冀凡,王会文,许振海.2004.冀北小寺沟铜钥矿外围银金资源潜力浅析[J].地质找矿丛论,19(1):20-23.
涂光炽.1989.关于超大型矿床的寻找和理论研究[J].地球科学进展,(6):14-20.
王强,许继锋,王建新,赵振华,王人镜,邱家骧,熊小林,桑隆康,彭练红.2000.大别山adakite岩型灰色片麻岩的确立及其与超高压变质作用的关系[J].科学通报,46(10):1017-1024.
王强,赵振华,熊小林,许继锋.2001.底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠英闪长玢岩的证据[J].地球化学,30(4):353-362.
王强,赵振华,许继峰,白正华,王建新,刘成新.2004.鄂东南铜山口、殷祖埃达克质(adakite)的侵入岩地球化学特征对比:(拆沉)下地壳熔融与斑岩铜矿的成因[J].岩石学报,20(2):351-360.
王焰,张旗,钱青.2000.埃达克岩(adakite)的地球化学特征及其构造意义[J].地质科学,35(2):251-256.
王元龙,张旗,王强,刘红涛,王焰.2003.埃达克质岩与Cu-Au成矿作用关系的初步探讨[J].岩石学报,19(3):543-550.
王元龙,王焰,张旗,贾秀琴,韩松.2004.铜陵地区中生代中酸性侵入岩的地球化学特征及其成矿———地球动力学意义[J]岩石学报,20:325-338.
肖庆辉,邓晋福,马大铨,洪大卫,莫宣学.2002.花岗岩研究思维与方法[M].北京:地质出版社.12-63.
许立权,邓晋福,陈志勇,陶继雄.2003.内蒙古达茂旗北部奥陶纪埃达克岩类的识别及其意义[J].现代地质,17(4):428-434.
尹冰川,冉清昌.1997.多宝山超大型铜矿床的成矿构造环境[J].矿物学报,17(2):220-224.
余良范,杨晓勇,孙卫东,池月余,张千明.2008.埃达克岩与皖中沙溪斑岩铜矿的成矿作用[J].中国地质,35(6):1150-1161.
翟裕生,张湖,宋鸿林.1997.大型构造与超大型矿床[M].北京:地质出版社.152-169.
张洪涛,陈仁义,韩芳林.2004.重新认识中国斑岩铜矿的成矿地质条件[J].矿床地质,23(2):150-163.
张旗,钱青,王二七,王焰,赵太平,郝杰,郭光军.2001a.燕山中晚期的中国东部高原:埃达克岩的启示[J].地质科学,36(2):248-255.
张旗,王焰,王元龙.2001b.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约[J].岩石学报,17(4):505-512.
张旗,王焰,刘红涛,王元龙,李之彤.2003a.中国埃达克岩的时空分布及其形成背景附:国内关于埃达克岩的争论[J].地学前缘,10(4):385-400.
张旗,王焰,王元龙.2003b.埃达克岩与构造环境[J].大地构造与成矿学,27(2):101-108.
张旗,许继峰,王焰,肖龙,刘红涛,王元龙.2004.埃达克岩的多样性[J].地质通报,23(9/l0):959-965.
张旗,金惟俊,王元龙,李承东,王焰,贾秀勤.2006.大洋岩石圈拆沉与大陆下地壳拆沉:不同的机制及意义———兼评“下地壳+岩石圈地幔拆沉模式”[J].岩石学报,22(11):2631-2738.
张旗.2008.埃达克岩研究的回顾和前瞻[J].中国地质,35(1):32-39.
赵文津.2007.大型斑岩铜矿成矿的深部构造岩浆活动背景[J].中国地质,34(2):179-205.
周刚,张招崇,罗世宾,何斌,王祥,应立娟,赵华,李爱红,贺永康.2007.新疆阿尔泰山南缘玛因鄂博高温型强过铝花岗岩:年龄、地球化学特征及其地质意义[J].岩石学报,23(8):1909-1020.
Batchlo R Aand Bowden P.1985.Petrogeneticinterpretationof granotoidrock series using multination parameters[J].Chem.Goel.,48(1/4):43-55.
Bo T B and Zhao B.1990.Geological and geochemical evidence of con-temporaneity and consanguinity of the Xiaosigou porphyry depositand its coexisting skarn deposits[J].Geochemical,2:166-174(in Chinese with English abstract).
Chappell B Wand White AJ R.1974.Two contrasting granitetype[J].Pacific Geology,173-174.
Chung S L,Liu D Y,Ji J Q,Chu MF,Lee H Y,Wen D J,Lo C H,Lee T Y,Qian Qand Zhang Q.2003.Adakites fromcontinentalcollision zone:Melting of thickened lower-crust beneath southeastTibet[J].Geology,31(11):1021-1024.
Defant MJ and Drummond MS.1990.Derivation of some modern arcmagmas by melting of young subduction lithosphere[J].Nature,347:662-665.
Defant MJ,Richerson M,De Boer J Z,Stewart R H,Maury R C,Bellon H,Drummond M S,Feigenson M D and Jackson T E.1991.Dacite genesis via both slab melting and differentiation:Pet-rogenesis of La Yeguada volcanic complex[J].Panama J.Petrol.,32:1101-1142.
Defant MJ and Drummond MS.1993.Mount St Helens:Potential ex-ample of the partial melting of the subductedlithospherein a volcanicarc[J].Geology,21:547-550.
DengJ F,Zhao HL,Mo X Xand Luo Z H.1996.The key of continen-tal root-pole tectonics and the dynamics in china[M].Beijing:Geol.Pub.House.1-110(in Chinese).
Deng J F,Zhao G C,Zhao J L,Luo Z H,Dai S Qand Li K M.2000.Yanshanian igneous petrotectonic assemblages and orogenic-deepprocessesin east China[J].Geological Review,46(1):41-48(inChinese with English abstract).
Dong S W,Wu X H,Wu Z H,Deng J F,Gao Yand Wang C S.2000.Ontectonic seesawing of the east Asia continent-global i mplication ofthe Yanshanian movement[J].Geological Review,46(1):8-13(inChinese with English abstract).
Drummond M S and Defant M J.1990.A model for trondhjemite-tonalite adakitic genesis and crustal growth via slab melting:Ar-chaean to modern comparisons[J].Geophys.Res.,95:21503-21521.
Fang WX,Yang S F,Liu Z T,Wei X L and Zhang B C.2007.Geo-chemical characteristics and significance of major element,trace ele-ments and REEin mineralized altered rocks of large scale TsagaanSuvarga Cu-Mo porphyry deposit in Mongolia[J].Journal of theChinese Rare Earth Society,25(1),85-94(in Chinese with Eng-lish abstract).
Gao B S and Zheng Y Y.2006.Geochemical controlling of mineraliza-tionin Qulong super-large porphyry copper deposit,Tibet[J].Geo-logical Science and Technology Information,25(2):41-46(in Chi-nese with English abstract).
Gregory A Davis.2003.The Yanshanian belt of north China:Tectonics,adakitic magmatism,and crustal evolution[J].Earth Science Fron-tiers,12(4):373-384.
Han X Land Yin LJ.1999.The study onthe ore-controlledfactors andmetallogenic regularity of Xiaosigou Cu-Mo deposit[J].Journal ofHebei Institute of Technology,21(2):62-66(in Chinese withEnglish abstract).
Hollister V F and Sirvas E B.1974.The Michiquillay porphyry copperdeposit[J].Mineraium Deposita,9(2):261-269.
Hollings P and Kerrich R.2000.An Archean arc basalt-Nb-enrichedbasalt-adakite association:The2.7Ga confederation assemblages ofthe Birch-Uchi greenstone belt,Superior Province[J].Contrions toMineralogy and Petrology,139:208-226.
Hou Z Q,Mo X X,Gao Y F,Qu X Mand Meng XJ.2003.Adakite,Apossible host rock for porphyry copper deposits:Case studies ofporphyry copper belts in Tibetan plateau and in northern Chile[J].Mineral Deposits,22(1):1-12(in Chinese with English abstract).
Hu XZ.1988.Discussion of characteristics and genesisin Yeji wei quartzporphyry rocks with tin[A].In:Huxiang Zhao Technology[C].Changsha:Central South University Press.24-30(in Chinese withEnglish abstract).
Isbibara S.1977.The magnetite-series andil menite-series granitic rocks[J].Mining Geology,27:293-305.
Kepezhinskas P K,Defant MJ and Drummond MS.1996.Progressiveenrichment of island arc mantle by melt-peridotite interaction in-ferred from Kamchatka xenoliths[J].Geochi m.Cosmochi m.Acta,60:1217-1229.
Li WC and Zeng P S.2007.Characteristics and metallogenic model ofthe Pulang super-large porphyry copper deposit in Yunnan,China[J].Journal of Chengdu University of Technology,34(4):436-446(in Chinese with English abstract).
Marc J D,Xu J F,Pavel K,Wang Q,Zhang Q and Xiao L.2002.Adakites:Some variations on a theme[J].Acta Petrologica Sinica,18(2):129-142.
Martin H.1999.Adakitic magmas:Modern analogues of Archaeangranitoids[J].Lithos,46:411-429.
Morris P A.1995.Slab melting as an explanation of Quaternary volcan-ismand aseismicity in southwestern Japan[J].Geology,23:395-398.
Nelson K D.1992.Are crustal thickness variations in old mountain beltlike the Appalachians a consequence of lithospheres delaminating[J]?Geology,20(06):498-502.
Patino Douce A E.1997.Generation of metal minerals:A-type granitesbylowpressure melting of calc-alkaline granitites[J].Geology,25(02):743-746.
Peacock S M,Rushmer Tand Thompson AB.1994.Partial melting ofsubducting oceanic crust[J].Earth Planet Sci.Lett.,121:227-244.
Peacock S Mand Wang K.1999.Seismic consequences of warmversuscool subduction metamorphism:Examples from southwest andnortheast Japan[J].Sciences,286:937-939.
Philip R Wand James F L.1998.Rare earth element metasomatisminhydrothermal systerms:The Willsboro-Lewis wollastonite ores,New York,USA[J].Geochem.Cosmochi m.Acta,62(17):2964-2968.
Qin J F,Lai S C and Li Y F.2007.Genesis of the Indosinian Guang-toushan adakitic biotite plagiogranite in the Mianxian-Lueyang(Mi-anlue)suture,south Qingling,and its tectonic i mplications[J].Geological Bulletin of China,26(4):466-471(in Chinese with Eng-lish abstract).
Rapp R P,Watson E Band Miller C F.1991.Partial melting of amphi-bolites ecologies and the origin of Achaean trend emits and tonalities[J].Precambrian Research,51(05):1-25.
Rapp R P and Watson E B.1995.Dehydration melting of metabasalt at8-32Kbar:I mplications for continental growth and crust-mantle re-cycling[J].Petrol.,36:891-931.
Rapp R P,Shi mizu Nand Norman MD.1999.Reaction between slab-derived melts and peridotiteinthe mantle wedge:Experi mental con-straints at3.8Gpa[J].Chemical Geology,160:335-356.
Rapp R P,Xiao L and Shi mizu N.2002.Experi mental constraints onthe origin of potassium-rich adakites in eastern China[J].ActaPetrologica Sinica,18(3):293-302.
Ren J S.1999.Tectonic map of China and adjacent region[M].Beijing:Geol.Pub.House.1-50(in Chinese).
Rui Z Y,Hang C K and Qi M G.1984.Porphyry copper(molybde-num)in China[M].Beijing:Geol.Pub.House.1-350(in Chi-nese).
Sen C and Dunn T.1994.Dehydration melting of a basaltic compositionamphibolite at1.5and2.0GPa:I mplications for the origin ofadakites[J].Contrib.Miner.Petrol.,117:394-409.
Sillitoe R H.1972.A plate tectonic model for the origin of porphyrycopper deposits[J].Econ.Geol.,67:184-197.
Springer Wand Seck HA.1997.Partial fusion of basic granulites at5to15Kbar:I mplications for the origin of TTG magmas[J].Contrib.Miner.Petrol.,127:30-45.
Stern C Rand Kilian R.1996.Role of the subductedslab,mantle wedgeand continental crust in the generation of adakites fromthe Australvolcanic zone[J].Contrib.Miner.Petrol.,123:263-281.
Sun J F,Wang H Wand Xu Z H.2004.Study on the Ag mineral re-source potential in the surrounding of Xiaosigou Cu-Mo deposit inthe north Hebei Province[J].Contributions to Geology and MineralResources Research,9(1):20-23(in Chinese with English ab-stract).
Sylverster P J.1998.Post-collision strongly peraluminous granites[J].Lithos,45:29-44.
Thieblemont D and Lehrberger J L.1997.Gisements epithermal andporphyry:A connection adakite[J].Earth Planet.Sci.Lett.,325:103-109.
Tu G Z.1989.Prospecting and theory about super-large deposits[J].Advancein Earth Sciences,6:14-20(in Chinese with English ab-stract).
Wang Q,Xu J F,Wang J X,Zhao Z H,Wang RJ,Qiu J X,Xiong XL,Sang L Kand Peng L H.2000.The recognition of adakite-typegneissesin the north Dabie Mountains and the relationship betweenthemand ultrahigh pressure metamorphism[J].Chinese ScienceBulletin,46(10):1017-1024(in Chinese).
Wang Q,Zhao Z H,Xiong X L and Xu J F.2001.Melting of the un-derplated basalticlower crust:Evidence fromthe Shaxi adakitic sod-ic quartz diorite-porphyrites,Anhui Province,China[J].Geochi mi-ca,30(4):353-362(in Chinese with English abstract).
Wang Q,Zhao Z H,Xu J F,Bai Z H,Wang J Xand Liu C X.2004.The geochemical comparison between the Tongshankou and Yinzuadakitic intrusive rocksin southeastern Hubei:(Delaminated)Low-er crustal melting and the genesis of porphyry copper deposit[J].Acta Petrologica Sinica,20(2):351-360(in Chinese with Englishabstract).
Wang Y,Zhang Qand Qian Q.2000.Adakite geochemical characteris-tics andtectonic significances[J].Scientia Geologica Sinica,35(2):251-256(in Chinese with English abstract).
Wang Y L,Zhang Q,Wang Q,Liu HTand Wang Y.2003.Study onadakitic rock and Cu-Au mineralization[J].Acta Petrologica Sinica,19(3):543-550(in Chinese with English abstract).
Wang Y L,Wang Y,Zhang Q,Jia X Qand Han S.2004.The geo-chemical characteristics of Mesozoic intermediate-acid intrusives ofthe Tongling area and its metallogenesis geodynamic i mplications[J].Acta Petrologica Sinica,20(2):325-338(in Chinese withEnglish abstract).
Xiao Q H,Deng F Q,Ma D S,Hong D Wand Mo X X.2002.Thethought and meanings in the granites research[M].Beijing:Geol.Pub.House.12-63(in Chinese).
Xie Q Q,Xu X C,Li X X,Cheng T Hand Lu S M.2006.Rare earthelements geochemistry of Laowan gold deposit in Henan Province:Trace to source of ore-forming materials[J].Journal of RareEarths,24(1):114-119
Xu J F,Shinjo R,Defant MJ and Wang Q.2002.Origin of Mesozoicadakitic intrusive rocks in the Ningzhen area of east China:Partialmelting of delaminated lower continental crust[J]?Geology,30:1111-1114.
Xu L Q,Deng J F,Chen Z Yand Tao J X.2003.Theidentification ofOrdovician adakites and its signification in northern Damao,innerMongolia[J].Geoscience,17(4):428-434(in Chinese with Eng-lish abstract).
Yin B C and Yan Q C.1997.The tectonic environments of metalloge-niesis of Duobaoshan super-large copper deposit[J].Acta Miner-alogica Sinica,17(2):220-224(in Chinese with English abstract).
Yogodzinski G M,Kay R W,Volynets O N,Kay S Mand Koloskov AV.1995.Magnesian andesiteinthe western Aleutian Komandorskyregion:I mplications for slab melting and processes in the mantlewedge[J].Geol.Society Am.Bull.,107:505-519.
Yu L F,Yang X Y,Sun WD,Chi Y Yand Zhang Q M.2008.Theadakite and mineralization of the Shaxi porphyry copper-gold de-posit,central Anhui[J].Geologyin China,35(6):1150-1161(inChinese with English abstract).
Zhai YS,Zhang Hand SongJ L.1997.Largetectonics andsuper-largedeposits[M].Beijing:Geol.Pub.House.152-169(in Chinese).
Zhang HT,Chen R Yand Han F L.2004.Re-understanding of metal-logenic geological conditions of porphyry copper deposits in China[J].Mineral Deposits,23(2):150-163(in Chinese with Englishabstract).
Zhang Q,Qian Q,Wang E C,Wang Y,Zaho TP,Hao J and Guo GJ.2001a.An east China plateauin mid-late Yanshanian period:I mpli-cation fromadakites[J].Chinese Journal of Geology,36(2):248-255(in Chinese with English abstract).
Zhang Q,Wang Y and Wang Y L.2001b.Preli minary study on thecomponents of the lower crust in east China Plateau during Yan-shani-an period:Constraints on Sr and Ndisotopic compositions ofadaklte-like rocks[J].Acta Petrologica Sinica,17(4):505-513(inChinese with English abstract).
Zhang Q,Wang Y,Liu H T,Wang Y L and Li Z T.2003a.On thespaceti me distribution and geodynamic environments of adakites inChina annex:Controversies over differing opinions for adakites inChina[J].Earth Science Frontiers,10(4):385-400(in Chinesewith English abstract).
Zhang Q,Wang Yand Wang Y L.2003b.Onthe relationship betweenAdakite andits tectonic setting[J].Geotectonica et Metallogenia,27(02):101-108(in Chinese with English abstract).
Zhang Q,Xu J F,Wang Y,Xiao L,Liu H T and Wang Y L.2004.Diversity of adakite[J].Geological Bulletin of China,23(9/l0):959-965(in Chinese with English abstract).
Zhang Q,Jin WJ,Wang Y L,Li C D,Wang Yand Jia X Q.2006.Ocean lithosphere delamination and the lower crust delamination:The different mechanism and geological i mplication:Comment onthe delamination model of lower crust and lithosphere mantle[J].Acta Petrologica Sinica,22(11):2631-2638(in Chinese with Eng-lish abstract).
Zhang Q.2008.Adakite research:Retrospect and prospect[J].Geologyin China,35(1):32-39(in Chinese with English abstract).
Zhao WJ.2007.Deep tectono-magmatic setting for metallogenesis oflarge porphyry copper deposits[J].Geologyin China,34(2):179-205(in Chinese with English abstract).
Zhou G,Zhang Z C,Luo S B,He B,Wang X,Ying LJ,Zhao H,Li AHand He Y K.2007.Confirmation of high-temperature stronglyperaluminous Mayin’ebo granitesinthe south margin of Altay,Xin-jiang:Age,geochemistry and tectonic i mplications[J].Acta Petro-logica Sinica,23(8):1909-1020(in Chinese with English ab-stract).
柏天宝,赵斌.1990.小寺沟斑岩矿床及其共生的矽卡岩矿床的周期性、同源性的地质地球化学证据[J].地球化学,(2):166-174.
邓晋福,赵海玲,莫宣学,罗照华.1996.中国大陆根-柱构造-大陆动力学的钥匙[M].北京:地质出版社.1-110.
邓晋福,赵国春,赵海玲,罗照华,戴圣潜,李凯明.2000.中国东部燕山期火成岩构造组合与造山深部过程[J].地质论评,46:41-48.
董树文,吴锡浩,吴珍汉,邓晋福,高锐,王成善.2000.论东亚大陆的构造翘变———燕山运动的全球意义[J].地质论评,46:8-13.
方维萱,杨杜锋,刘正桃,韦星林,张宝琛.2007.蒙古查干苏布尔加(Tsagaan Suvarga)大型斑岩型铜钼矿床含矿蚀变岩常量、微量和稀土元素地球化学特征及意义[J].中国稀土学报,25(1):85-94.
高宝顺,郑有业.2006.西藏驱龙超大型斑岩铜矿床成矿作用的地球化学控制[J].地质科技情报,25(2):41-46.
韩秀丽,尹力军.1999.小寺沟铜钼矿床控矿因素及成矿规律[J].河北理工学院学报,21(2):62-66.
候增谦,莫宣学,高永丰,曲晓明,孟祥金.2003.埃达克岩:斑岩铜矿的一种可能的重要含矿母岩[J].矿床地质,22(1):1-12.
胡祥昭.1988.野鸡尾含锡石英斑岩的岩石学特征及成因探讨[A].胡祥昭论文集[C].长沙:中南大学出版社.24-30.
李文昌,曾普胜.2007.云南普朗超大型斑岩铜矿特征及成矿模型[J].成都理工大学学报,34(4):436-446.
秦江峰,赖绍聪,李永飞.2007.南秦岭勉县-略阳缝合带印支期光头山埃达克质花岗岩的成因及其地质意义[J].地质通报,26(4):466-471.
任纪舜.1999.中国及邻区大地构造图[M].北京:地质出版社.1-50.
芮宗瑶,黄崇轲,齐国明.1984.中国斑岩铜(钼)矿床[M].北京:地质出版社.1-350.
孙冀凡,王会文,许振海.2004.冀北小寺沟铜钥矿外围银金资源潜力浅析[J].地质找矿丛论,19(1):20-23.
涂光炽.1989.关于超大型矿床的寻找和理论研究[J].地球科学进展,(6):14-20.
王强,许继锋,王建新,赵振华,王人镜,邱家骧,熊小林,桑隆康,彭练红.2000.大别山adakite岩型灰色片麻岩的确立及其与超高压变质作用的关系[J].科学通报,46(10):1017-1024.
王强,赵振华,熊小林,许继锋.2001.底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠英闪长玢岩的证据[J].地球化学,30(4):353-362.
王强,赵振华,许继峰,白正华,王建新,刘成新.2004.鄂东南铜山口、殷祖埃达克质(adakite)的侵入岩地球化学特征对比:(拆沉)下地壳熔融与斑岩铜矿的成因[J].岩石学报,20(2):351-360.
王焰,张旗,钱青.2000.埃达克岩(adakite)的地球化学特征及其构造意义[J].地质科学,35(2):251-256.
王元龙,张旗,王强,刘红涛,王焰.2003.埃达克质岩与Cu-Au成矿作用关系的初步探讨[J].岩石学报,19(3):543-550.
王元龙,王焰,张旗,贾秀琴,韩松.2004.铜陵地区中生代中酸性侵入岩的地球化学特征及其成矿———地球动力学意义[J]岩石学报,20:325-338.
肖庆辉,邓晋福,马大铨,洪大卫,莫宣学.2002.花岗岩研究思维与方法[M].北京:地质出版社.12-63.
许立权,邓晋福,陈志勇,陶继雄.2003.内蒙古达茂旗北部奥陶纪埃达克岩类的识别及其意义[J].现代地质,17(4):428-434.
尹冰川,冉清昌.1997.多宝山超大型铜矿床的成矿构造环境[J].矿物学报,17(2):220-224.
余良范,杨晓勇,孙卫东,池月余,张千明.2008.埃达克岩与皖中沙溪斑岩铜矿的成矿作用[J].中国地质,35(6):1150-1161.
翟裕生,张湖,宋鸿林.1997.大型构造与超大型矿床[M].北京:地质出版社.152-169.
张洪涛,陈仁义,韩芳林.2004.重新认识中国斑岩铜矿的成矿地质条件[J].矿床地质,23(2):150-163.
张旗,钱青,王二七,王焰,赵太平,郝杰,郭光军.2001a.燕山中晚期的中国东部高原:埃达克岩的启示[J].地质科学,36(2):248-255.
张旗,王焰,王元龙.2001b.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约[J].岩石学报,17(4):505-512.
张旗,王焰,刘红涛,王元龙,李之彤.2003a.中国埃达克岩的时空分布及其形成背景附:国内关于埃达克岩的争论[J].地学前缘,10(4):385-400.
张旗,王焰,王元龙.2003b.埃达克岩与构造环境[J].大地构造与成矿学,27(2):101-108.
张旗,许继峰,王焰,肖龙,刘红涛,王元龙.2004.埃达克岩的多样性[J].地质通报,23(9/l0):959-965.
张旗,金惟俊,王元龙,李承东,王焰,贾秀勤.2006.大洋岩石圈拆沉与大陆下地壳拆沉:不同的机制及意义———兼评“下地壳+岩石圈地幔拆沉模式”[J].岩石学报,22(11):2631-2738.
张旗.2008.埃达克岩研究的回顾和前瞻[J].中国地质,35(1):32-39.
赵文津.2007.大型斑岩铜矿成矿的深部构造岩浆活动背景[J].中国地质,34(2):179-205.
周刚,张招崇,罗世宾,何斌,王祥,应立娟,赵华,李爱红,贺永康.2007.新疆阿尔泰山南缘玛因鄂博高温型强过铝花岗岩:年龄、地球化学特征及其地质意义[J].岩石学报,23(8):1909-1020.
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