西藏达布矿区含矿岩体的时代、岩石地球化学特征及岩石成因
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摘要
达布矿区位于冈底斯成矿带中段南侧,具较大的铜(钼)成矿潜力.通过对达布矿区含矿花岗闪长岩体开展岩石学、LAICP-MS锆石U-Pb定年和岩石地球化学等方面的分析研究,结果显示达布矿区花岗闪长岩体是主要的含矿岩体之一,其LAICP-MS锆石U-Pb年龄为16.5±0.3 Ma~16.0±0.4 Ma,属中新世(N1).岩体具高Al(Al_2O_3=15.6%~16.5%)、高Na(Na_2O=4.51%~4.82%)、钙碱性系列、弱过铝质;稀土元素具弱正铕异常(Eu/Eu*=1.02~1.27)和正铈异常(Ce/Ce*=0.99~1.53);富集Rb、Ba、Sr和亏损Nb、Ta、Ti、Y.达布矿区花岗闪长岩体属I型花岗岩,类似于典型的C型埃达克岩,明显有别于冈底斯带中新世高K埃达克岩;为印度-亚洲大陆碰撞后局部伸展背景下,由加厚下地壳物质(石榴石角闪岩)较高程度部分熔融的岩浆产物.
Dabu mining area is located in the southern part of the middle Gangdese metallogenic belt,which has great metallogenic potential of Cu(Mo)deposit.In this paper,petrology,LA-ICP-MS zircon U-Pb dating,rock geochemistry of the Dabu ore-bearing granodiorite body are systematically studied.The results suggest that the Dabu granodiorite pluton is one of the major ore-bearing rock body,and its LA-ICP-MS zircon U-Pb age is 16.5±0.3 Ma-16.0±0.4 Ma,with the corresponding age of Miocene(N1).The rock mass has high Al(Al_2O_3 =15.6%-16.5%),high Na(Na_2O=4.51%-4.82%),and it is calc-alkaline and weakly peraluminous.REE elements have weak positive Eu anomalies(Eu/Eu*=1.02-1.27)and positive Ce anomalies(Ce/Ce*=0.99-1.53).Trace elements ratio spider diagram displays apparent enrichments of Rb,Ba,Sr and marked depletions of Nb,Ta,Ti,Y.The Dabu granodiorite pluton belongs to I-type granite,which is similar to the typical C-type adakite,but is obviously different from the Miocene high-K adakite in the Gangdese belt.It is concluded that Dabu granodiorite pluton is a relatively high degree of partial melting of the thickened lower crust material(garnet amphibolite)formed in the background of partial extension of the India Asian continent post-collision.
Dabu mining area is located in the southern part of the middle Gangdese metallogenic belt,which has great metallogenic potential of Cu(Mo)deposit.In this paper,petrology,LA-ICP-MS zircon U-Pb dating,rock geochemistry of the Dabu ore-bearing granodiorite body are systematically studied.The results suggest that the Dabu granodiorite pluton is one of the major ore-bearing rock body,and its LA-ICP-MS zircon U-Pb age is 16.5±0.3 Ma-16.0±0.4 Ma,with the corresponding age of Miocene(N1).The rock mass has high Al(Al_2O_3 =15.6%-16.5%),high Na(Na_2O=4.51%-4.82%),and it is calc-alkaline and weakly peraluminous.REE elements have weak positive Eu anomalies(Eu/Eu*=1.02-1.27)and positive Ce anomalies(Ce/Ce*=0.99-1.53).Trace elements ratio spider diagram displays apparent enrichments of Rb,Ba,Sr and marked depletions of Nb,Ta,Ti,Y.The Dabu granodiorite pluton belongs to I-type granite,which is similar to the typical C-type adakite,but is obviously different from the Miocene high-K adakite in the Gangdese belt.It is concluded that Dabu granodiorite pluton is a relatively high degree of partial melting of the thickened lower crust material(garnet amphibolite)formed in the background of partial extension of the India Asian continent post-collision.
引文
Altherr,R.,Holl,A.,Hegner,E.,et al.,2000.High-Potassium,Calc-Alkaline I-Type Plutonism in the European Variscides:Northern Vosges(France)and Northern Schwarzwald(Germany).Lithos,50(1-3):51-73.https://doi.org/10.1016/s0024-4937(99)00052-3
Batchelor,R.A.,Bowden,P.,1985.Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters.Chemical Geology,48(1-4):43-55.https://doi.org/10.1016/0009-2541(85)90034-8
Chappell,B.W.,White,A.J.R,1974.Two Contrasting Granite Type.Pacific Geology,8:173-174.
Collins,W.J.,Beams,S.D.,White,A.J.R.,et al.,1982.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia.Contributions to Mineralogy and Petrology,80(2):189-200.https://doi.org/10.1007/bf00374895
Cox,K.G.,Bell,J.D.,Pankhurst,R.J.,1979.The Interpretation of Igneous Rocks.Allen and Unwin,London.
Defant,M.J.,Drummond,M.S.,1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature,347(6294):662-665.https://doi.org/10.1038/347662a0
DePaolo,D.J.,Daley,E.E.,2000.Neodymium Isotopes in Basalts of the Southwest Basin and Range and Lithospher-ic Thinning during Continental Extension.Chemical Geology,169(1-2):157-185.https://doi.org/10.1016/s0009-2541(00)00261-8
Drummond,M.S.,Defant,M.J.,1990.A Model for TrondhjemiteTonalite-Dacite Genesis and Crustal Growth via Slab Melting:Archean to Modern Comparisons.Journal of Geophysical Research Solid Earth,95(B13):21503-21521.https://doi.org/10.1029/JB095iB13p21503
Gao,Y.M.,Chen,Y.C.,Tang,J.X.,et al.,2012.A Study of Diagenetic and Metallogenic Geochronology of the Dagbo Cu(Mo)Deposit in Quxur County of Tibet and Its Geological Implications.Acta Geoscientica Sinica,33(4):613-623(in Chinese with English abstract).
Geng,R.R.,2014.Characteristics of Ore-Forming Fluid of Dabu Porphyry Cu-Mo Deposit in Tibet(Dissertation).China University of Geosciences,Beijing(in Chinese with English abstract).
Hoskin,P.W.O.,2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62.https://doi.org/10.2113/0530027
Hou,Z.Q.,Gao,Y.F.,Meng,X.J.,et al.,2004.Genesis of Adaltitic Porphyry and Tectonic Controls on the Gangdese Miocene Porphyry Copper Belt in the Tibetan Orogen.Acta Petrologica Sinica,20(2):239-248(in Chinese with English abstract).
Hou,Z.Q.,Meng,X.J.,Qu,X.M.,et al.,2005.Copper Ore Potential of Adakitic Intrusives in Gangdese Porphyry Copper Belt:Constrains from Rock Phase and Deep Melting Process.Mineral Deposits,24(2):108-121(in Chinese with English abstract).
Hou,Z.Q.,Mo,X.X.,Gao,Y.F.,et al.,2003a.Adakite,APossible Host Rock for Porphyry Copper Deposits:Case Studies of Porphyry Copper Belts in Tibetan Plateau and in Northern Chile.Mineral Deposits,22(1):1-12(in Chinese with English abstract).
Hou,Z.Q.,Mo,X.X.,Gao,Y.F.,et al.,2006.Early Processes and Tectonic Model for the Indian-Asian Contiental Collision Evidence from the Cenozoic Gangdese Igneous Rocks in Tibet.Acta Geologica Sinica,80(9):1233-1248(in Chinese with English abstract).
Hou,Z.Q.,Qu,X.M.,Wang,S.X.,et al.,2003b.Re-Os Ages of Molybdenite in the Gangdese Porphyry Copper Belt in South Tibet:Duration of Mineralization and Application of the Dynamic Setting.Science in China(Series D),33(7):609-618(in Chinese).
Irvine,T.N.,Baragar,W.R.A.,1971.A Guide to the Chemical Classification of the Common Volcanic Rocks.CanadianJournal of Earth Sciences,8(5):523-548.https://doi.org/10.1139/e71-055
Ji,W.Q.,Wu,F.Y.,Zhong,S.L,et al.,2009.Geochronology and Petrogenesis of Granitic Rocks in Gangdese Batholiths,Southern Tibet.Science in China(Series D),39(7):849-871(in Chinese).
Kay,S.M.,Mpodozis,C.,2001.Central Andean Ore Deposits Linked to Evolving Shallow Subduction Systems and Thickening Crust.GSA Today,11(3):4.https://doi.org/10.1130/1052-5173(2001)011<0004:caodlt>2.0.co;2
Lai,S.C.,Qin,J.F.,Zhu,R.Z.,et al.,2015.Petrogenesis and Tectonic Implication of the Neoproterozoic Peraluminous Granitoids from the Tianquan Area,Western Yangtze Block,South China.Acta Petrologica Sinica,31(8):2245-2258(in Chinese with English abstract).
Leng,Q.F.,Tang,J.X.,Zheng,W.B.,et al.,2016.Geochronology,Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakange Porphyry Cu-Mo Deposit,Tibet.Earth Science,41(6):999-1015(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2016.083
Li,G.M.,Duan,Z.M.,Huang,Y.,et al.,2017.GangdeseHimalayan Geology and Mineralization in Tibet.China University of Geosciences Press,Wuhan(in Chinese).
Li,G.M.,Rui,Z.Y.,2004.Diagenetic and Mineralization Ages for the Porphyry Copper Deposits in the Gangdise Metallogenic Belt,Southern Xizang.Geotectonica et Metallogenia,28(2):165-170(in Chinese with English abstract).
Li,Y.W.,Wei,Q.R.,Wang,C.,et al.,2017.Zircon U-Pb Dating and Geochemistry of Late Triassic Intermediate Dykes in Suyingdi,Eastern Section of West Kunlun and Their Geological Significance.Earth Science,42(6):909-926(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.083
Liu,Y.S.,Hu,Z.C.,Gao,S.,et al.,2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology,257(1-2):34-43.https://doi.org/10.1016/j.chemgeo.2008.08.004
Lu,F.X.,Sang,L.K.,2002.Petrology.Geological Publishing House,Beijing,93-94(in Chinese).
Ludwig,K.R.,2003.Users Manual for Isoplot 3.6:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center,Berkeley.
Maniar,P.D.,Piccoli,P.M.,1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin,101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
Mao,X.L.,Wang,G.Z.,Chen,J.J.,et al.,2013.Comparison of Geochemical Characteristics of Granite Porphyry and Typical Adakitic Rocks in the Dabu Area,Tibet,China.Acta Mineralogica Sinica,(S2):341-342(in Chinese).
Meng,X.J.,2004.The Metallogeny of the Miocene Gangdese Porphyry Copper Belt in Tibetan Collisional Orogen(Dissertation).Chinese Academy of Geological Sciences,Beijing(in Chinese with English abstract).
Meng,Y.K.,2016.Tectonic Evolution of the Southern Region in the Middle Gangdese Batholith,Southern Tibet(Dissertation).Chinese Academy of Geological Sciences,Beijing(in Chinese with English abstract).
Middlemost,E.A.K.,1975.The Basalt Clan.Earth-Science Reviews,11(4):337-364.https://doi.org/10.1016/0012-8252(75)90039-2
Middlemost,E.A.K.,1985.Magmas and Magmatic Rocks:An Introduction to Igneous Petrology.Longman,New York.
Misra,K.C.,1999.Understanding Mineral Deposits.Kluwer Academic Publishers,New York,353-413.
Mo,X.X.,Pan,G.T.,2006.From the Tethys to the Formation of the Qinghai Tibet Plateau:Constrained by Tectone Magmatic Events.Earth Science Frontiers,13(6):43-51(in Chinese with English abstract).
Mo,X.X.,Zhao,Z.D.,Deng,J.F.,et al.,2003.Response of Volcanism to the India Asia Conllision.Earth Science Frontiers,10(3):135-148(in Chinese with English abstract).
Moyen,J.F.,2009.High Sr/Y and La/Yb Ratios:The Meaning of the“Adakitic Signature”.Lithos,112(3-4):556-574.https://doi.org/10.1016/jl.ithos.2009.04.001
Mungall,J.E.,2002.Roasting the Mantle:Slab Melting and the Genesis of Major Au and Au-Rich Cu Deposits.Geology,30(10):915.https://doi.org/10.1130/0091-7613(2002)030<0915:rtmsma>2.0.co;2
Pan,G.T.,Mo,X.X.,Hou,Z.Q.,et al.,2006.SpatialTemporal Framework of the Gangdese Orogenic Belt and Its Evolution.Acta Petrologica Sinica,22(3):521-533(in Chinese with English abstract).
Pan,G.T.,2013.Tectonic Maps and Manuals of the QinghaiTibet Plateau and Its Adjacent Areas.Geological Publishing House,Beijing(in Chinese).
Peccerillo,A.,Taylor,S.R.,1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area,Northern Turkey.Contributions to Mineralogy and Petrology,58(1):63-81.https://doi.org/10.1007/bf00384745
Qu,X.M.,Hou,Z.Q.,Huang,W.,2001.Is Gangdese Porphyry Copper Belt the Second“Yulong”Copper Belt?Mineral Deposits,20(4):355-366(in Chinese withEnglish abstract).
Qu,X.M.,Hou,Z.Q.,Xin,H.B.,2006.Zircon SHRIMP Ages and Geochemical Characteristics of Two Generations of Adakite from Gangdese Collisional Orogenic Belt,Tibet.Mineral Deposits,(S1):419-422(in Chinese).
Rapp,R.P.,Watson,E.B.,1995.Dehydration Melting of Metabasalt at 8-32kbar:Implications for Continental Growth and Crust-Mantle Recycling.Journal of Petrology,36(4):891-931.https://doi.org/10.1093/petrology/36.4.891
Reich,M.,Parada,M.A.,Palacios,C.,et al.,2003.AdakiteLike Signature of Late Miocene Intrusions at the Los Pelambres Giant Porphyry Copper Deposit in the Andes of Central Chile:Metallogenic Implications.Mineralium Deposita,38(7):876-885.https://doi.org/10.1007/s00126-003-0369-9
Rui,Z.Y.,Li,G.M.,Wang,L.S.,2004.Metallic Mineral Resources on the Qinghai-Tibet Plateau.Geological Bulletin of China,23(1):20-23(in Chinese).
Rui,Z.Y.,Zhang,H.T.,Chen,R Y.,et al.,2006.An Approach to Some Problems of Porphyry Copper Deposits.Mineral Deposits,25(4):491-500(in Chinese with English abstract).
Sang,L.K.,Ma,C.Q.,2012.Petrology(Second Edition).Geological Publishing House,Beijing,188(in Chinese).
Sun,S.S.,McDonough,W.F.,1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society,London,Special Publications,42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19
Tang,J.X.,Duo,J.,Liu,H.F.,et al.,2012.Minerogenetic Series of Ore Deposits in the East Part of the Gangdese Metallogenic Belt.Acta Geoscientica Sinica,33(4):393-410(in Chinese with English abstract).
Wang,Q.,Xu,J.F.,Zhao,Z.H.,2001.The Summary and Comment on Research on a New Kind of Igneous Rock-Adakite.Advance in Earth Sciences,16(2):201-208(in Chinese with English abstract).
Wang,Y.Y.,Tang,J.X.,Zheng,W.B.,et al.,2015.Mechanism of Metal Precipitation in Dabu Porphyry Cu-Mo Deposit,Quxu Country,Tibet.Mineral Deposits,34(1)81-97(in Chinese with English abstract).
Wu,F.Y.,Huang,B.C.,Ye,K.,et al.,2008.Collapsed Himalayan-Tibetan Orogen and the Rising Tibetan Plateau.Acta Petrologica Sinica,24(1):1-30(in Chinese with English abstract).
Wu,Y.B.,Zheng,Y.F.,2004.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age.Chinese ScienceBulletin,49(16):1589-1604(in Chinese).
Xia,B.B.,Xia,B.,Wang,B.D.,et al.,2007.Ore-Bearing Adakitic Porphyry in the Middle of Gangdese:Thickened Lower Crustal Melting and the Genesis of Porphyry Cu-Mo Deposit.Geological Science and Technology Information,26(4):19-26(in Chinese with English abstract).
Xiong,X.L.,Adam,J.,Green,T.H.,2005.Rutile Stability and Rutile/Melt HFSE Partitioning during Partial Melting of Hydrous Basalt:Implications for TTG Genesis.Chemical Geology,218(3-4):339-359.https://doi.org/10.1016/j.chemgeo.2005.01.014
Yang,Z.,Jiang,H.,Yang,M.G.,et al.,2017.Zircon U-Pb and Molybdenite Re-Os Dating of the Gangjiang Porphyry Cu-Mo Deposit in Central Gangdese and Its Geological Significance.Earth Science,42(03):339-356(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.026
Zhang,Q.,Wang,Y.,Qian,Q.,et al.,2001.The Characteristics and Tectonic-Metallogenic Significances of the Adakites in Yanshan Period from Eastern China.Acta Petrologica Sinica,17(2):236-244(in Chinese with English abstract).
Zheng,G.F.,Zhong,K.H.,Gou,J.,et al.,2011.Geology and Prospecting of Dabu Porphyry Cu-Mo Type Deposit of Qushui Country in Tibet.Sichuan Nonferrous Metals,(3):9-13(in Chinese with English abstract).
Zheng,Y.Y.,Xue,Y.X.,Cheng,L.J.,et al.,2004.Finding,Characteristics and Significances of Qulong Superlarge Porphyry Copper(Molybdenum)Deposit,Tibet.Earth Science,29(1):103-108(in Chinese with English abstract).https://doi.org/10.3321/j.issn:1000-2383.2004.01.018
Zheng,Y.Y.,Zhang,G.Y.,Xu,R.K.,et al.,2007.Geochronolosic Constraints on Masmatic Intrusions and Mineralization of the Zhunuo Porphyry Copper Deposit in Gangdese,Tibet.Chinese Science Bulletin,52(21):2542-2548(in Chinese).
Zhu,D.C.,Duan,L.P.,Liao,Z.L.,et al.,2002.Discrimination for Two Kinds of Adakites.Journal of Mineralogy and Petrology,22(3):5-9(in Chinese with English abstract).
高一鸣,陈毓川,唐菊兴,等,2012.西藏曲水县达布斑岩铜(钼)矿床成岩成矿年代学研究.地球学报,33(4):613-623.
耿瑞瑞,2014.西藏达布斑岩铜钼矿床成矿流体特征(硕士学位论文).北京:中国地质大学.
侯增谦,高永丰,孟祥金,等,2004.西藏冈底斯中新世斑岩铜矿带:埃达克质斑岩成因与构造控制.岩石学报,20(2):239-248.
侯增谦,孟祥金,曲晓明,等,2005.西藏冈底斯斑岩铜矿带埃达克质斑岩含矿性:源岩相变及深部过程约束.矿床地质,24(2):108-121.
侯增谦,莫宣学,高永丰,等,2003a.埃达克岩:斑岩铜矿的一种可能的重要含矿母岩---以西藏和智利斑岩铜矿为例.矿床地质,22(1):1-12.
侯增谦,莫宣学,高永丰,等,2006.印度大陆与亚洲大陆早期碰撞过程与动力学模型---来自西藏冈底斯新生代火成岩证据.地质学报,80(9):1233-1248.
侯增谦,曲晓明,王淑贤,等,2003b.西藏高原冈底斯斑岩铜矿带辉钼矿Re-Os年龄:成矿作用时限与动力学背景应用.中国科学(D辑),33(7):609-618.
纪伟强,吴福元,锺孙霖,等,2009.西藏南部冈底斯岩基花岗岩时代与岩石成因.中国科学(D辑),39(7):849-871.
赖绍聪,秦江锋,朱韧之,等,2015.扬子地块西缘天全新元古代过铝质花岗岩类成因机制及其构造动力学背景.岩石学报,31(8):2245-2258.
冷秋锋,唐菊兴,郑文宝,等,2016.西藏拉抗俄斑岩Cu-Mo矿床含矿斑岩地球化学、锆石U-Pb年代学及Hf同位素组成.地球科学,41(6):999-1015.
李光明,段志明,黄勇,等,2017.西藏冈底斯-喜马拉雅地质与成矿.武汉:中国地质大学出版社.
李光明,芮宗瑶,2004.西藏冈底斯成矿带斑岩铜矿的成岩成矿年龄.大地构造与成矿学,28(2):165-170.
黎有为,魏启荣,王程,等,2017.西昆仑东段宿营地晚三叠世中性脉岩的锆石U-Pb定年、岩石地球化学特征及其意义.地球科学,42(6):909-926.
路凤香,桑隆康,2002.岩石学.北京:地质出版社,93-94.
毛秀丽,王国芝,陈俊瑾,等,2013.西藏达布地区花岗斑岩与典型埃达克岩地球化学特征对比浅析.矿物学报,(S2):341-342.
孟祥金,2004.西藏碰撞造山带冈底斯中新世斑岩铜矿成矿作用研究(博士学位论文).北京:中国地质科学院.
孟元库,2016.藏南冈底斯中段南缘构造演化(博士学位论文).北京:中国地质科学院.
莫宣学,潘桂棠,2006.从特提斯到青藏高原形成:构造-岩浆事件的约束.地学前缘,13(6):43-51.
莫宣学,赵志丹,邓晋福,等,2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘,10(3):135-148.
潘桂棠,2013.青藏高原及邻区大地构造图及说明书.北京:地质出版社.
潘桂棠,莫宣学,侯增谦,等,2006.冈底斯造山带的时空结构及演化.岩石学报,22(3):521-533.
曲晓明,侯增谦,黄卫,2001.冈底斯斑岩铜矿(化)带:西藏第二条“玉龙”铜矿带?矿床地质,20(4):355-366.
曲晓明,侯增谦,辛洪波,2006.西藏冈底斯碰撞造山带两套埃达克岩的锆石SHRIMPU-Pb年龄及地球化学特征.矿床地质,(S1):419-422.
芮宗瑶,李光明,王龙生,2004.青藏高原的金属矿产资源.地质通报,23(1):20-23.
芮宗瑶,张洪涛,陈仁义,等,2006.斑岩铜矿研究中若干问题探讨.矿床地质,25(4):491-500.
桑隆康,马昌前,2012.岩石学(第二版).北京:地质出版社,188.
唐菊兴,多吉,刘鸿飞,等,2012.冈底斯成矿带东段矿床成矿系列及找矿突破的关键问题研究.地球学报,33(4):393-410.
王强,许继锋,赵振华,2001.一种新的火成岩---埃达克岩的研究综述.地球科学进展,16(2):201-208.
王艺云,唐菊兴,郑文宝,等,2015.西藏曲水县达布斑岩型铜钼矿床金属沉淀机制探讨.矿床地质,34(1):81-97.
吴福元,黄宝春,叶凯,等,2008.青藏高原造山带的垮塌与高原隆升.岩石学报,24(1):1-30.
吴元宝,郑永飞,2004.锆石成因矿物学研究及其U-Pb年龄解释的制约.科学通报,49(16):1589-1604.
夏抱本,夏斌,王保弟,等,2007.冈底斯中段达布埃达克质含矿斑岩:增厚下地壳熔融与斑岩铜钼矿成因.地质科技情报,26(4):19-26.
杨震,姜华,杨明国,等,2017.冈底斯中段岗讲斑岩铜钼矿床锆石U-Pb和辉钼矿Re-Os年代学及其地质意义.地球科学,42(3):339-356.
张旗,王焰,钱青,等,2001.中国东部燕山期埃达克岩的特征及其构造-成矿意义.岩石学报,17(2):236-244.
郑高峰,钟康惠,苟金,等,2011.西藏曲水县达布斑岩型铜钼矿床地质特征及找矿前景.四川有色金属,(3):9-13.
郑有业,薛迎喜,程力军,等,2004.西藏驱龙超大型斑岩铜(钼)矿床:发现、特征及意义.地球科学,29(1):103-108.
郑有业,张刚阳,许荣科,等,2007.西藏冈底斯朱诺斑岩铜矿床成岩成矿时代约束.科学通报,52(21):2542-2548.
朱弟成,段丽萍,廖忠礼,等,2002.两类埃达克岩(Adakite)的判别.矿物岩石,22(3):5-9.
Batchelor,R.A.,Bowden,P.,1985.Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters.Chemical Geology,48(1-4):43-55.https://doi.org/10.1016/0009-2541(85)90034-8
Chappell,B.W.,White,A.J.R,1974.Two Contrasting Granite Type.Pacific Geology,8:173-174.
Collins,W.J.,Beams,S.D.,White,A.J.R.,et al.,1982.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia.Contributions to Mineralogy and Petrology,80(2):189-200.https://doi.org/10.1007/bf00374895
Cox,K.G.,Bell,J.D.,Pankhurst,R.J.,1979.The Interpretation of Igneous Rocks.Allen and Unwin,London.
Defant,M.J.,Drummond,M.S.,1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature,347(6294):662-665.https://doi.org/10.1038/347662a0
DePaolo,D.J.,Daley,E.E.,2000.Neodymium Isotopes in Basalts of the Southwest Basin and Range and Lithospher-ic Thinning during Continental Extension.Chemical Geology,169(1-2):157-185.https://doi.org/10.1016/s0009-2541(00)00261-8
Drummond,M.S.,Defant,M.J.,1990.A Model for TrondhjemiteTonalite-Dacite Genesis and Crustal Growth via Slab Melting:Archean to Modern Comparisons.Journal of Geophysical Research Solid Earth,95(B13):21503-21521.https://doi.org/10.1029/JB095iB13p21503
Gao,Y.M.,Chen,Y.C.,Tang,J.X.,et al.,2012.A Study of Diagenetic and Metallogenic Geochronology of the Dagbo Cu(Mo)Deposit in Quxur County of Tibet and Its Geological Implications.Acta Geoscientica Sinica,33(4):613-623(in Chinese with English abstract).
Geng,R.R.,2014.Characteristics of Ore-Forming Fluid of Dabu Porphyry Cu-Mo Deposit in Tibet(Dissertation).China University of Geosciences,Beijing(in Chinese with English abstract).
Hoskin,P.W.O.,2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry,53(1):27-62.https://doi.org/10.2113/0530027
Hou,Z.Q.,Gao,Y.F.,Meng,X.J.,et al.,2004.Genesis of Adaltitic Porphyry and Tectonic Controls on the Gangdese Miocene Porphyry Copper Belt in the Tibetan Orogen.Acta Petrologica Sinica,20(2):239-248(in Chinese with English abstract).
Hou,Z.Q.,Meng,X.J.,Qu,X.M.,et al.,2005.Copper Ore Potential of Adakitic Intrusives in Gangdese Porphyry Copper Belt:Constrains from Rock Phase and Deep Melting Process.Mineral Deposits,24(2):108-121(in Chinese with English abstract).
Hou,Z.Q.,Mo,X.X.,Gao,Y.F.,et al.,2003a.Adakite,APossible Host Rock for Porphyry Copper Deposits:Case Studies of Porphyry Copper Belts in Tibetan Plateau and in Northern Chile.Mineral Deposits,22(1):1-12(in Chinese with English abstract).
Hou,Z.Q.,Mo,X.X.,Gao,Y.F.,et al.,2006.Early Processes and Tectonic Model for the Indian-Asian Contiental Collision Evidence from the Cenozoic Gangdese Igneous Rocks in Tibet.Acta Geologica Sinica,80(9):1233-1248(in Chinese with English abstract).
Hou,Z.Q.,Qu,X.M.,Wang,S.X.,et al.,2003b.Re-Os Ages of Molybdenite in the Gangdese Porphyry Copper Belt in South Tibet:Duration of Mineralization and Application of the Dynamic Setting.Science in China(Series D),33(7):609-618(in Chinese).
Irvine,T.N.,Baragar,W.R.A.,1971.A Guide to the Chemical Classification of the Common Volcanic Rocks.CanadianJournal of Earth Sciences,8(5):523-548.https://doi.org/10.1139/e71-055
Ji,W.Q.,Wu,F.Y.,Zhong,S.L,et al.,2009.Geochronology and Petrogenesis of Granitic Rocks in Gangdese Batholiths,Southern Tibet.Science in China(Series D),39(7):849-871(in Chinese).
Kay,S.M.,Mpodozis,C.,2001.Central Andean Ore Deposits Linked to Evolving Shallow Subduction Systems and Thickening Crust.GSA Today,11(3):4.https://doi.org/10.1130/1052-5173(2001)011<0004:caodlt>2.0.co;2
Lai,S.C.,Qin,J.F.,Zhu,R.Z.,et al.,2015.Petrogenesis and Tectonic Implication of the Neoproterozoic Peraluminous Granitoids from the Tianquan Area,Western Yangtze Block,South China.Acta Petrologica Sinica,31(8):2245-2258(in Chinese with English abstract).
Leng,Q.F.,Tang,J.X.,Zheng,W.B.,et al.,2016.Geochronology,Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakange Porphyry Cu-Mo Deposit,Tibet.Earth Science,41(6):999-1015(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2016.083
Li,G.M.,Duan,Z.M.,Huang,Y.,et al.,2017.GangdeseHimalayan Geology and Mineralization in Tibet.China University of Geosciences Press,Wuhan(in Chinese).
Li,G.M.,Rui,Z.Y.,2004.Diagenetic and Mineralization Ages for the Porphyry Copper Deposits in the Gangdise Metallogenic Belt,Southern Xizang.Geotectonica et Metallogenia,28(2):165-170(in Chinese with English abstract).
Li,Y.W.,Wei,Q.R.,Wang,C.,et al.,2017.Zircon U-Pb Dating and Geochemistry of Late Triassic Intermediate Dykes in Suyingdi,Eastern Section of West Kunlun and Their Geological Significance.Earth Science,42(6):909-926(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.083
Liu,Y.S.,Hu,Z.C.,Gao,S.,et al.,2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology,257(1-2):34-43.https://doi.org/10.1016/j.chemgeo.2008.08.004
Lu,F.X.,Sang,L.K.,2002.Petrology.Geological Publishing House,Beijing,93-94(in Chinese).
Ludwig,K.R.,2003.Users Manual for Isoplot 3.6:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center,Berkeley.
Maniar,P.D.,Piccoli,P.M.,1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin,101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
Mao,X.L.,Wang,G.Z.,Chen,J.J.,et al.,2013.Comparison of Geochemical Characteristics of Granite Porphyry and Typical Adakitic Rocks in the Dabu Area,Tibet,China.Acta Mineralogica Sinica,(S2):341-342(in Chinese).
Meng,X.J.,2004.The Metallogeny of the Miocene Gangdese Porphyry Copper Belt in Tibetan Collisional Orogen(Dissertation).Chinese Academy of Geological Sciences,Beijing(in Chinese with English abstract).
Meng,Y.K.,2016.Tectonic Evolution of the Southern Region in the Middle Gangdese Batholith,Southern Tibet(Dissertation).Chinese Academy of Geological Sciences,Beijing(in Chinese with English abstract).
Middlemost,E.A.K.,1975.The Basalt Clan.Earth-Science Reviews,11(4):337-364.https://doi.org/10.1016/0012-8252(75)90039-2
Middlemost,E.A.K.,1985.Magmas and Magmatic Rocks:An Introduction to Igneous Petrology.Longman,New York.
Misra,K.C.,1999.Understanding Mineral Deposits.Kluwer Academic Publishers,New York,353-413.
Mo,X.X.,Pan,G.T.,2006.From the Tethys to the Formation of the Qinghai Tibet Plateau:Constrained by Tectone Magmatic Events.Earth Science Frontiers,13(6):43-51(in Chinese with English abstract).
Mo,X.X.,Zhao,Z.D.,Deng,J.F.,et al.,2003.Response of Volcanism to the India Asia Conllision.Earth Science Frontiers,10(3):135-148(in Chinese with English abstract).
Moyen,J.F.,2009.High Sr/Y and La/Yb Ratios:The Meaning of the“Adakitic Signature”.Lithos,112(3-4):556-574.https://doi.org/10.1016/jl.ithos.2009.04.001
Mungall,J.E.,2002.Roasting the Mantle:Slab Melting and the Genesis of Major Au and Au-Rich Cu Deposits.Geology,30(10):915.https://doi.org/10.1130/0091-7613(2002)030<0915:rtmsma>2.0.co;2
Pan,G.T.,Mo,X.X.,Hou,Z.Q.,et al.,2006.SpatialTemporal Framework of the Gangdese Orogenic Belt and Its Evolution.Acta Petrologica Sinica,22(3):521-533(in Chinese with English abstract).
Pan,G.T.,2013.Tectonic Maps and Manuals of the QinghaiTibet Plateau and Its Adjacent Areas.Geological Publishing House,Beijing(in Chinese).
Peccerillo,A.,Taylor,S.R.,1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area,Northern Turkey.Contributions to Mineralogy and Petrology,58(1):63-81.https://doi.org/10.1007/bf00384745
Qu,X.M.,Hou,Z.Q.,Huang,W.,2001.Is Gangdese Porphyry Copper Belt the Second“Yulong”Copper Belt?Mineral Deposits,20(4):355-366(in Chinese withEnglish abstract).
Qu,X.M.,Hou,Z.Q.,Xin,H.B.,2006.Zircon SHRIMP Ages and Geochemical Characteristics of Two Generations of Adakite from Gangdese Collisional Orogenic Belt,Tibet.Mineral Deposits,(S1):419-422(in Chinese).
Rapp,R.P.,Watson,E.B.,1995.Dehydration Melting of Metabasalt at 8-32kbar:Implications for Continental Growth and Crust-Mantle Recycling.Journal of Petrology,36(4):891-931.https://doi.org/10.1093/petrology/36.4.891
Reich,M.,Parada,M.A.,Palacios,C.,et al.,2003.AdakiteLike Signature of Late Miocene Intrusions at the Los Pelambres Giant Porphyry Copper Deposit in the Andes of Central Chile:Metallogenic Implications.Mineralium Deposita,38(7):876-885.https://doi.org/10.1007/s00126-003-0369-9
Rui,Z.Y.,Li,G.M.,Wang,L.S.,2004.Metallic Mineral Resources on the Qinghai-Tibet Plateau.Geological Bulletin of China,23(1):20-23(in Chinese).
Rui,Z.Y.,Zhang,H.T.,Chen,R Y.,et al.,2006.An Approach to Some Problems of Porphyry Copper Deposits.Mineral Deposits,25(4):491-500(in Chinese with English abstract).
Sang,L.K.,Ma,C.Q.,2012.Petrology(Second Edition).Geological Publishing House,Beijing,188(in Chinese).
Sun,S.S.,McDonough,W.F.,1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society,London,Special Publications,42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19
Tang,J.X.,Duo,J.,Liu,H.F.,et al.,2012.Minerogenetic Series of Ore Deposits in the East Part of the Gangdese Metallogenic Belt.Acta Geoscientica Sinica,33(4):393-410(in Chinese with English abstract).
Wang,Q.,Xu,J.F.,Zhao,Z.H.,2001.The Summary and Comment on Research on a New Kind of Igneous Rock-Adakite.Advance in Earth Sciences,16(2):201-208(in Chinese with English abstract).
Wang,Y.Y.,Tang,J.X.,Zheng,W.B.,et al.,2015.Mechanism of Metal Precipitation in Dabu Porphyry Cu-Mo Deposit,Quxu Country,Tibet.Mineral Deposits,34(1)81-97(in Chinese with English abstract).
Wu,F.Y.,Huang,B.C.,Ye,K.,et al.,2008.Collapsed Himalayan-Tibetan Orogen and the Rising Tibetan Plateau.Acta Petrologica Sinica,24(1):1-30(in Chinese with English abstract).
Wu,Y.B.,Zheng,Y.F.,2004.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age.Chinese ScienceBulletin,49(16):1589-1604(in Chinese).
Xia,B.B.,Xia,B.,Wang,B.D.,et al.,2007.Ore-Bearing Adakitic Porphyry in the Middle of Gangdese:Thickened Lower Crustal Melting and the Genesis of Porphyry Cu-Mo Deposit.Geological Science and Technology Information,26(4):19-26(in Chinese with English abstract).
Xiong,X.L.,Adam,J.,Green,T.H.,2005.Rutile Stability and Rutile/Melt HFSE Partitioning during Partial Melting of Hydrous Basalt:Implications for TTG Genesis.Chemical Geology,218(3-4):339-359.https://doi.org/10.1016/j.chemgeo.2005.01.014
Yang,Z.,Jiang,H.,Yang,M.G.,et al.,2017.Zircon U-Pb and Molybdenite Re-Os Dating of the Gangjiang Porphyry Cu-Mo Deposit in Central Gangdese and Its Geological Significance.Earth Science,42(03):339-356(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2017.026
Zhang,Q.,Wang,Y.,Qian,Q.,et al.,2001.The Characteristics and Tectonic-Metallogenic Significances of the Adakites in Yanshan Period from Eastern China.Acta Petrologica Sinica,17(2):236-244(in Chinese with English abstract).
Zheng,G.F.,Zhong,K.H.,Gou,J.,et al.,2011.Geology and Prospecting of Dabu Porphyry Cu-Mo Type Deposit of Qushui Country in Tibet.Sichuan Nonferrous Metals,(3):9-13(in Chinese with English abstract).
Zheng,Y.Y.,Xue,Y.X.,Cheng,L.J.,et al.,2004.Finding,Characteristics and Significances of Qulong Superlarge Porphyry Copper(Molybdenum)Deposit,Tibet.Earth Science,29(1):103-108(in Chinese with English abstract).https://doi.org/10.3321/j.issn:1000-2383.2004.01.018
Zheng,Y.Y.,Zhang,G.Y.,Xu,R.K.,et al.,2007.Geochronolosic Constraints on Masmatic Intrusions and Mineralization of the Zhunuo Porphyry Copper Deposit in Gangdese,Tibet.Chinese Science Bulletin,52(21):2542-2548(in Chinese).
Zhu,D.C.,Duan,L.P.,Liao,Z.L.,et al.,2002.Discrimination for Two Kinds of Adakites.Journal of Mineralogy and Petrology,22(3):5-9(in Chinese with English abstract).
高一鸣,陈毓川,唐菊兴,等,2012.西藏曲水县达布斑岩铜(钼)矿床成岩成矿年代学研究.地球学报,33(4):613-623.
耿瑞瑞,2014.西藏达布斑岩铜钼矿床成矿流体特征(硕士学位论文).北京:中国地质大学.
侯增谦,高永丰,孟祥金,等,2004.西藏冈底斯中新世斑岩铜矿带:埃达克质斑岩成因与构造控制.岩石学报,20(2):239-248.
侯增谦,孟祥金,曲晓明,等,2005.西藏冈底斯斑岩铜矿带埃达克质斑岩含矿性:源岩相变及深部过程约束.矿床地质,24(2):108-121.
侯增谦,莫宣学,高永丰,等,2003a.埃达克岩:斑岩铜矿的一种可能的重要含矿母岩---以西藏和智利斑岩铜矿为例.矿床地质,22(1):1-12.
侯增谦,莫宣学,高永丰,等,2006.印度大陆与亚洲大陆早期碰撞过程与动力学模型---来自西藏冈底斯新生代火成岩证据.地质学报,80(9):1233-1248.
侯增谦,曲晓明,王淑贤,等,2003b.西藏高原冈底斯斑岩铜矿带辉钼矿Re-Os年龄:成矿作用时限与动力学背景应用.中国科学(D辑),33(7):609-618.
纪伟强,吴福元,锺孙霖,等,2009.西藏南部冈底斯岩基花岗岩时代与岩石成因.中国科学(D辑),39(7):849-871.
赖绍聪,秦江锋,朱韧之,等,2015.扬子地块西缘天全新元古代过铝质花岗岩类成因机制及其构造动力学背景.岩石学报,31(8):2245-2258.
冷秋锋,唐菊兴,郑文宝,等,2016.西藏拉抗俄斑岩Cu-Mo矿床含矿斑岩地球化学、锆石U-Pb年代学及Hf同位素组成.地球科学,41(6):999-1015.
李光明,段志明,黄勇,等,2017.西藏冈底斯-喜马拉雅地质与成矿.武汉:中国地质大学出版社.
李光明,芮宗瑶,2004.西藏冈底斯成矿带斑岩铜矿的成岩成矿年龄.大地构造与成矿学,28(2):165-170.
黎有为,魏启荣,王程,等,2017.西昆仑东段宿营地晚三叠世中性脉岩的锆石U-Pb定年、岩石地球化学特征及其意义.地球科学,42(6):909-926.
路凤香,桑隆康,2002.岩石学.北京:地质出版社,93-94.
毛秀丽,王国芝,陈俊瑾,等,2013.西藏达布地区花岗斑岩与典型埃达克岩地球化学特征对比浅析.矿物学报,(S2):341-342.
孟祥金,2004.西藏碰撞造山带冈底斯中新世斑岩铜矿成矿作用研究(博士学位论文).北京:中国地质科学院.
孟元库,2016.藏南冈底斯中段南缘构造演化(博士学位论文).北京:中国地质科学院.
莫宣学,潘桂棠,2006.从特提斯到青藏高原形成:构造-岩浆事件的约束.地学前缘,13(6):43-51.
莫宣学,赵志丹,邓晋福,等,2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘,10(3):135-148.
潘桂棠,2013.青藏高原及邻区大地构造图及说明书.北京:地质出版社.
潘桂棠,莫宣学,侯增谦,等,2006.冈底斯造山带的时空结构及演化.岩石学报,22(3):521-533.
曲晓明,侯增谦,黄卫,2001.冈底斯斑岩铜矿(化)带:西藏第二条“玉龙”铜矿带?矿床地质,20(4):355-366.
曲晓明,侯增谦,辛洪波,2006.西藏冈底斯碰撞造山带两套埃达克岩的锆石SHRIMPU-Pb年龄及地球化学特征.矿床地质,(S1):419-422.
芮宗瑶,李光明,王龙生,2004.青藏高原的金属矿产资源.地质通报,23(1):20-23.
芮宗瑶,张洪涛,陈仁义,等,2006.斑岩铜矿研究中若干问题探讨.矿床地质,25(4):491-500.
桑隆康,马昌前,2012.岩石学(第二版).北京:地质出版社,188.
唐菊兴,多吉,刘鸿飞,等,2012.冈底斯成矿带东段矿床成矿系列及找矿突破的关键问题研究.地球学报,33(4):393-410.
王强,许继锋,赵振华,2001.一种新的火成岩---埃达克岩的研究综述.地球科学进展,16(2):201-208.
王艺云,唐菊兴,郑文宝,等,2015.西藏曲水县达布斑岩型铜钼矿床金属沉淀机制探讨.矿床地质,34(1):81-97.
吴福元,黄宝春,叶凯,等,2008.青藏高原造山带的垮塌与高原隆升.岩石学报,24(1):1-30.
吴元宝,郑永飞,2004.锆石成因矿物学研究及其U-Pb年龄解释的制约.科学通报,49(16):1589-1604.
夏抱本,夏斌,王保弟,等,2007.冈底斯中段达布埃达克质含矿斑岩:增厚下地壳熔融与斑岩铜钼矿成因.地质科技情报,26(4):19-26.
杨震,姜华,杨明国,等,2017.冈底斯中段岗讲斑岩铜钼矿床锆石U-Pb和辉钼矿Re-Os年代学及其地质意义.地球科学,42(3):339-356.
张旗,王焰,钱青,等,2001.中国东部燕山期埃达克岩的特征及其构造-成矿意义.岩石学报,17(2):236-244.
郑高峰,钟康惠,苟金,等,2011.西藏曲水县达布斑岩型铜钼矿床地质特征及找矿前景.四川有色金属,(3):9-13.
郑有业,薛迎喜,程力军,等,2004.西藏驱龙超大型斑岩铜(钼)矿床:发现、特征及意义.地球科学,29(1):103-108.
郑有业,张刚阳,许荣科,等,2007.西藏冈底斯朱诺斑岩铜矿床成岩成矿时代约束.科学通报,52(21):2542-2548.
朱弟成,段丽萍,廖忠礼,等,2002.两类埃达克岩(Adakite)的判别.矿物岩石,22(3):5-9.