云南中甸地区翁水晚三叠世火山岩地球化学特征及其构造意义
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摘要
"三江"构造带中甸弧北部的印支期岩浆活动目前尚无正式的研究报道。本文的岩石学及年代学的研究表明,中甸弧北部的翁水地区存在印支期中酸性岩浆活动,锆石U-Pb定年结果显示这些火山岩在211.1±1.5Ma喷发,与该地区的印支期火山岩与斑岩矿床的成矿斑岩的形成时代一致。翁水安山岩岩石地球化学特征显示其以中性的安山岩为主,具有亏损Nb、Ta、Ti等高场强元素的典型岛弧岩浆成分特征。与同一构造单元内中甸弧南部的烂泥塘-浪都安山岩进行主、微量元素的对比研究发现,两者均具有正常岛弧火山岩的成分组成特征。结合其形成时代和构造背景,初步认为中甸弧北部的翁水和南部的烂泥塘-浪都安山岩以及该区域的成矿斑岩很可能形成于同一构造-岩浆事件,都是甘孜-理塘洋晚三叠世俯冲作用的岩浆产物。
It has not been reported at presen0t of arc magmatic activities for Late Triassic in northern zhongdian arc of Sanjiang tectonic belt. Our petrological and chronological researches show that the intermediate-acid magmatic activity of Indosinian developed in Wengshui areas of Zhongdian arc; zircon U-Pb dating indicates that the volcanic rocks in Wengshui area were erupted at 211.1±1.5Ma, which is similar to ages of other Indosinian volcanic rocks and ore-bearing porphyric rocks in southern Zhongdian area. The Wengshui volcanic rocks mainly consist of andesites and show depletion of high field strength elements such as Nb, Ta, Ti similar to arc volcanic rocks. Compared with Lannitang-Langdu andesites from southern area of Zhongdian arc, the both clearly show compositional signature of an arc volcanic rock. Combining their age and tectonic background, we conclude that Wengshui andesites, Lannitang-Langdu andesites and ore-bearing porphyric rocks from Zhongdian area were most likely formed by a same tectono-magmatic event, which were generated by westward subduction of the Ganzi-Litang in Late-Triassic.
It has not been reported at presen0t of arc magmatic activities for Late Triassic in northern zhongdian arc of Sanjiang tectonic belt. Our petrological and chronological researches show that the intermediate-acid magmatic activity of Indosinian developed in Wengshui areas of Zhongdian arc; zircon U-Pb dating indicates that the volcanic rocks in Wengshui area were erupted at 211.1±1.5Ma, which is similar to ages of other Indosinian volcanic rocks and ore-bearing porphyric rocks in southern Zhongdian area. The Wengshui volcanic rocks mainly consist of andesites and show depletion of high field strength elements such as Nb, Ta, Ti similar to arc volcanic rocks. Compared with Lannitang-Langdu andesites from southern area of Zhongdian arc, the both clearly show compositional signature of an arc volcanic rock. Combining their age and tectonic background, we conclude that Wengshui andesites, Lannitang-Langdu andesites and ore-bearing porphyric rocks from Zhongdian area were most likely formed by a same tectono-magmatic event, which were generated by westward subduction of the Ganzi-Litang in Late-Triassic.
引文
Cao DH,Wang AJ,Huang YF et al.2009.SHRIMP geochronology andHf isotope composition of zircons from Xuejiping porphyry copperdeposit,Yunnan Province.Acta Geologica Sinica,83(10):1430-1435(in Chinese with English abstract)
Chen JL,Xu JF,Wang BD et al.2010.Origin of Cenozoic alkalinepotassic volcanic rocks at KonglongXiang,Lhasa terrane,TibetanPlateau:Products of partial melting of a mafic lower-crustal source?Chemical Geology,273(3-4):286-299
Chen JL,Xu JF,Ren JB et al.2011.Geochemical differences betweenthe subduction-and collisional-type ore-bearing porphyric rocks.Acta Petrologica Sinica,27(9):2733-2742(in Chinese withEnglish abstract)
Chen YQ,Huang JN and Liang Z.2008.Geochemical characteristics andzonation of primary halos of Pulang porphyry copper deposit,northwestern Yunnan Province,southwestern China.Journal ofChina University of Geosciences,19(4):371-377
Guo X,Du YS,Pang ZS et al.2009.Characteristics of the ore-formingfluids in alteration zones of the Pulang porphyry cupper deposit inYunnan Province and its metallogenic significance.Geoscience,23(3):465-471(in Chinese with English abstract)
Hastie AR,Kerr AC,Pearce JA and Mitchell SF.2007.Classification ofaltered volcanic island arc rocks using immobile trace elements:Development of the Th-Co discrimination diagram.Journal ofPetrology,48(12):2341-2357
Hoskin PWO and Schaltegger U.2003.The composition of zircon andigneous and metamorphic petrogenesis.Reviews in Mineralogy andGeochemistry,53(1):27-62
Hou ZQ and Mo XX.1991.The evolution of Yidun island-arc andimplications in the exploration of Kuroko-type volcanogenic massive sulphide deposits in Sanjiang area,China.Earth Science,16(2):154-164(in Chinese with English abstract)
Hou ZQ,Qu XM,Zhou JR et al.2001.Collision-orogenic processes ofthe Yidun arc in the Sanjiang Region:Record of granites.ActaGeologica Sinica,75(4):484-497(in Chinese with Englishabstract)
Hou ZQ,Yang YQ,Qu XM et al.2004.Tectonic evolution andmineralization systems of the Yidun arc orogen in Sanjiang region,China.Acta Geologica Sinica,78(1):109-120(in Chinese withEnglish abstract)
Huang XL,Xu YG,Lan JB et al.2009.Neoproterozoic adakitic rocksfrom Mopanshan in the western Yangtze Craton:Partial melts of athickened lower crust.Lithos,112(3-4):367-381
Huang XX,Xu JF,Chen JL et al.2012.Geochronology,geochemistryand petrogenesis of two periods of intermediate-acid intrusive rocksfrom Hongshan area in Zhongdian arc.Acta Petrologica Sinica,28(5):1493-1506(in Chinese with English abstract)
Li JK,Li WC,Wang DH et al.2007.Re-Os dating for ore-forming eventin the late of Yanshan Epoch and research of ore-forming regularity inZhongdian Arc.Acta Petrologica Sinica,23(10):2415-2422(inChinese with English abstract)
Li WC.2007.The tectonic evolution of the Yidun island arc and themetallogenic model of the Pulang porphyry copper deposit,Yunnan,SW China.Ph.D.Dissertation.Beijing:China University ofGeosciences(in Chinese with English summary)
Li WC,Yin GH,Lu YX et al.2009.The evolution and40Ar-39Arisotopic evidence of the Pulang complex in Zhongdian.ActaGeologica Sinica,83(10):1421-1429(in Chinese with Englishabstract)
Li WC,Zeng PS,Hou ZQ et al.2011.The Pulang porphyry copperdeposit and associated felsic intrusions in Yunnan Province,Southwest China.Economic Geologists,105(1):79-92
Li WC,Yin GH,Yu HJ et al.2011.The porphyry metallogenesis ofGeza volcanic magmatic arc in NW Yunnan.Acta Petrologica Sinica,27(9):2541-2552(in Chinese with English abstract)
Lin QC,Xia B and Zhang YQ.2006.Zircon SHRIMP U-Pb dating of thesyn-collisional Xuejiping quartz diorite porphyrite in Zhongdian,Yunnan,China,and its geological implications.Geological Bulletinof China,25(1-2):133-137(in Chinese with English abstract)
Liu XL.2009.Zhongdian island arc magmatic rocks geochemicalcharacteristics and porphyry copper mineralization.Master DegreeThesis.Kunming:Kunming University of Science and Technology(in Chinese with English summary)
Liu YS,Hu ZC,Gao S et al.2008.In situ analysis of major and traceelements of anhydrous minerals by LA-ICP-MS without applying aninternal standard.Chemical Geology,257(1-2):34-43
Liu YS,Gao S,Hu ZC et al.2010.Continental and oceanic crustrecycling-induced melt-peridotite interactions in the Trans-NorthChina Orogen:U-Pb dating,Hf isotopes and trace elements inzircons from mantle xenoliths.Journal of Petrology,51(1-2):537-571
Ludwig KR.2003.User’s Manual for Isoplot3.00:A GeochronologicalToolkit for Microsoft Excel.California:BerkeleyGeochronology Center
Mo XX,Lu FX,Hou ZQ et al.1993.Sanjiang Tethyan Volcanism andRelated Mineralization.Beijing:Geological Publishing House,266-267(in Chinese)
Pan GT,Ding J,Wang LQ et al.2005.The1∶1500000Geological MapSpecification of Qinghai-Tibet Plateau and Its Adjacent Area.3.Chengdu:Chengdu Map Publishing House,266-267(in Chinese)
Pang ZS,Du YS,Wang GW et al.2009.Single-grain zircon U-Pbisotopic ages,geochemistry and its implication of the Pulang complexin Yunnan Province,China.Acta Petrologica Sinica,25(1):159-165(in Chinese with English abstract)
Pearce JA.1983.Role of the sub-continental lithosphere in magmagenesis at active continental margins.In:Hawkesworth CJ and NorryMJ(eds.).Continental Basalts and Mantle Xenoliths.NantwichCheshire:Shiva Publications,230-249
Qu XM and Hou ZQ.2002.40Ar/39Ar age of the Panyong pillow basalt:Implication for the evolution relationship between the Jinshajiang andGarze-Litang suture zones.Geological Review,48(Suppl.):115-121(in Chinese with English abstract)
Reid AJ,Wilson CJL and Liu S.2005.Structural evidence for thePermo-Triassic tectonic evolution of the Yidun Arc,eastern TibetanPlateau.Journal of Structural Geology,27(1):119-137
Reid AJ,Wilson CJL,Liu S et al.2007.Mesozoic plutons of the Yidunarc,SW China:U/Pb geochronology and Hf isotopic signature.OreGeology Review,31(1-4):88-106
Ren JB.2011.The chronology,geochemistry and mineraliziongsignificance of porphyry copper deposits in Zhongdian island arc.Master Degree Thesis.Beijing:Graduate School of Chinese Academyof Sciences(in Chinese with English summary)
Ren JB,Xu JF,Chen JL et al.2011a.Geochemistry and petrogenesis ofPulang porphyries in Sanjiang region.Acta Petrologica etMineralogica,30(4):581-592(in Chinese with English abstract)
Ren JB,Xu JF and Chen JL.2011b.Zircon geochronology and geologicalimplications of ore-bearing porphyries from Zhongdian arc.ActaPetrologica Sinica,27(9):2591-2599(in Chinese with Englishabstract)
Ren T,Zhong H,Chen JF et al.2011.Geochemical characteristics ofthe Langdu high-K intermediate-acid intrusive rocks in the Zhongdianarea,Northwest Yunnan Province,P.R.China.Acta MineralogicaSinica,31(1):43-54(in Chinese with English abstract)
Sun SS and McDonough WF.1989.Chemical and isotopic systematics ofoceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in OceanicBasins.Geological Society,London,Special Publication,42(1):313-345
Wang BQ,Zhou MF,Li JW et al.2011.Late Triassic porphyriticintrusions and associated volcanic rocks from the Shangri-La region,Yidun terrane,eastern Tibetan Plateau:Adakitic magmatism andporphyry copper mineralization.Lithos,127(1-2):24-38
Wang SX.Zhang XC,Qin CJ et al.2007.Fuild inclusions in quartzveins of Pulang porphyry copper deposit,Zhongdian,northwesternYunnan,China.Geochimica,36(5):467-478(in Chinese withEnglish abstract)
Wang XF,Metcalfe I,Jian P et al.2000.The Jinshajiang-Ailaoshansuture zone,China:Tectonostratigraphy,age and evolution.Journalof Asian Earth Sciences,18(6):675-690
Wang XS,Bi XW,Leng CB et al.2011.LA-ICP-MS zircon U-Pb datingof granite porphyry in the Hongshan Cu-polymetallic deposit,Zhongdian,Northwest Yunnan,China and its geological implication.Acta Mineralogica Sinica,31(3):315-321(in Chinese withEnglish abstract)
Winchester JA and Floyd PA.1977.Geochemical discrimination ofdifferent magma series and their differentiation products usingimmobile elements.Chemical Geology,20:325-343
Wood DA.1980.The application of a Th-Hf-Ta diagram to problems oftectonomagmatic classification and to establishing the nature ofcrustal contamination of basaltic lavas of the British Tertiary VolcanicProvince.Earth and Planetary Science Letters,50(1):11-30
Yang TN,Hou ZQ,Wang Y et al.2012.Late Paleozoic to EarlyMesozoic tectonic evolution of northeast Tibet:Evidence from theTriassic composite western Jinsha-Garzê-Litang suture.Tectonics,31(4):1-20
Yang YQ,Hou ZQ,Huang DA et al.2002.Collision orogenic processand magmatic metallogenic system in Zhongdian arc.ActaGeoscientia Sinica,23(1):17-24(in Chinese with Englishabstract)
Zeng PS,Mo XX,Yu XH et al.2003.Porphyries and porphyry copperdeposits in Zhongdian area,northwestern Yunnan.MineralDeposits,22(4):393-400(in Chinese with English abstract)
Zeng PS,Hou ZQ,Wang HP et al.2004.Re-Os dating of the Pulangporphyry copper deposit in Zhongdian,NW Yunnan,and itsgeological significance.Acta Geologica Sinica,78(2):604-609
Zeng PS,Wang HP,Mo XX et al.2004.Tectonic setting and prospects of porphyry copper deposits in Zhongdian island arc belt.ActaGeoscientica Sinica,25(5):535-540(in Chinese with Englishabstract)
Zeng PS,Li WC,Wang HP et al.2006.The indosinian Pulangsuperlarge porphyry copper deposit in Yunnan,China:Petrology andchronology.Acta Petrologica Sinica,22(4):989-1000(inChinese with English abstract)
Zhang ZM and Jin M.1979.Two kinds of melange and their tectonicsignificance in Xiangcheng-Derong area,southwestern Sichuan.Scientia Geologica Sinica,(3):205-214
曹殿华,王安建,黄玉凤等.2009.中甸弧雪鸡坪斑岩铜矿含矿斑岩锆石SHRIMP U-Pb年代学及Hf同位素组成.地质学报,83(10):1430-1435
陈建林,许继峰,任江波等.2011.俯冲型和碰撞型含矿斑岩地球化学组成的差异.岩石学报,27(9):2733-2742
郭欣,杜杨松,庞振山等.2009.云南普朗斑岩铜矿蚀变带成矿流体特征及其成矿意义.现代地质,23(3):465-471
侯增谦,莫宣学.1991.义敦岛弧的形成演化及其对“三江”地区块状硫化物矿床的控制作用.地球科学,16(2):154-164
侯增谦,曲晓明,周继荣等.2001.三江地区义敦岛弧碰撞造山过程:花岗岩记录.地质学报,75(4):484-497
侯增谦,杨岳清,曲晓明等.2004.三江地区义敦岛弧造山带演化和成矿系统.地质学报,78(1):109-120
黄肖潇,许继峰,陈建林等.2012.中甸岛弧红山地区两期中酸性侵入岩的年代学、地球化学特征及其成因.岩石学报,28(5):1493-1506
李建康,李文昌,王登红等.2007.中甸弧燕山晚期成矿事件的Re-Os定年及成矿规律研究.岩石学报,23(10):2415-2422
李文昌.2007.义敦岛弧构造演化与普朗超大型斑岩铜矿成矿模型.博士学位论文.北京:中国地质大学
李文昌,尹光候,卢映祥等.2009.中甸普朗复式斑岩体演化及40Ar-39Ar同位素依据.地质学报,83(10):1421-1429
李文昌,尹光侯,余海军等.2011.滇西北格咱火山-岩浆弧斑岩成矿作用.岩石学报,27(9):2541-2552
林清茶,夏斌,张玉泉.2006.云南中甸地区雪鸡坪同碰撞石英闪长玢岩锆石SHRIMP U-Pb定年及其意义.地质通报,25(1-2):133-137
刘学龙.2009.中甸岛弧岩浆岩地球化学特征及斑岩型铜矿成矿研究.硕士学位论文.昆明:昆明理工大学
莫宣学,路凤香,侯增谦等.1993.三江特提斯火山作用与成矿.北京:地质出版社,266-267
潘桂堂,丁俊,王立全等.2005.青藏高原及邻区地质图(1∶1500000)说明书.3.成都:成都地图出版社,75-76
庞振山,杜杨松,王功文等.2009.云南普朗复式岩体锆石U-Pb年龄和地球化学特征及其地质意义.岩石学报,25(1):159-165
曲晓明,侯增谦.2002.从潘拥枕状玄武岩的40Ar/39Ar年龄论金沙江缝合带和甘孜-理塘缝合带的演化关系.地质评论,48(增刊):115-121
任江波.2011.中甸岛弧成矿斑岩和矿床的年代学、地球化学研究.硕士学位论文.北京:中国科学院研究生院
任江波,许继峰,陈建林等.2011a.“三江”地区中甸弧普朗成矿斑岩地球化学特征及其成因.岩石矿物学杂志,30(4):581-592
任江波,许继峰,陈建林.2011b.中甸岛弧成矿斑岩的锆石年代学及其意义.岩石学报,27(9):2591-2599
任涛,钟宏,陈金法等.2011.云南中甸地区浪都高钾中酸性侵入岩的地球化学特征.矿物学报,31(1):43-54
王守旭,张兴春,秦朝建等.2007.滇西北中甸普朗斑岩铜矿流体包裹体初步研究.地球化学,36(5):467-478
王新松,毕献武,冷成彪等.2011.滇西北中甸红山Cu多金属矿床花岗斑岩锆石LA-ICP-MS U-Pb定年及其地质意义.矿物学报,31(3):315-321
杨岳清,侯增谦,黄典豪等.2002.中甸弧碰撞造山作用和岩浆成矿系统.地球学报,23(1):12-24
曾普胜,莫宣学,喻学惠等.2003.滇西北中甸斑岩及斑岩铜矿.矿床地质,22(4):393-400
曾普胜,王海平,莫宣学等.2004.中甸岛弧带构造格架及斑岩铜矿前景.地球学报,25(5):535-540
曾普胜,李文昌,王海平等.2006.云南普朗印支期超大型斑岩铜矿床:岩石学及年代学特征.岩石学报,22(4):989-1000
张之孟,金蒙.1979.川西南乡城-得荣地区的两种混杂岩及其构造意义.地质科学,(3):206-214
Chen JL,Xu JF,Wang BD et al.2010.Origin of Cenozoic alkalinepotassic volcanic rocks at KonglongXiang,Lhasa terrane,TibetanPlateau:Products of partial melting of a mafic lower-crustal source?Chemical Geology,273(3-4):286-299
Chen JL,Xu JF,Ren JB et al.2011.Geochemical differences betweenthe subduction-and collisional-type ore-bearing porphyric rocks.Acta Petrologica Sinica,27(9):2733-2742(in Chinese withEnglish abstract)
Chen YQ,Huang JN and Liang Z.2008.Geochemical characteristics andzonation of primary halos of Pulang porphyry copper deposit,northwestern Yunnan Province,southwestern China.Journal ofChina University of Geosciences,19(4):371-377
Guo X,Du YS,Pang ZS et al.2009.Characteristics of the ore-formingfluids in alteration zones of the Pulang porphyry cupper deposit inYunnan Province and its metallogenic significance.Geoscience,23(3):465-471(in Chinese with English abstract)
Hastie AR,Kerr AC,Pearce JA and Mitchell SF.2007.Classification ofaltered volcanic island arc rocks using immobile trace elements:Development of the Th-Co discrimination diagram.Journal ofPetrology,48(12):2341-2357
Hoskin PWO and Schaltegger U.2003.The composition of zircon andigneous and metamorphic petrogenesis.Reviews in Mineralogy andGeochemistry,53(1):27-62
Hou ZQ and Mo XX.1991.The evolution of Yidun island-arc andimplications in the exploration of Kuroko-type volcanogenic massive sulphide deposits in Sanjiang area,China.Earth Science,16(2):154-164(in Chinese with English abstract)
Hou ZQ,Qu XM,Zhou JR et al.2001.Collision-orogenic processes ofthe Yidun arc in the Sanjiang Region:Record of granites.ActaGeologica Sinica,75(4):484-497(in Chinese with Englishabstract)
Hou ZQ,Yang YQ,Qu XM et al.2004.Tectonic evolution andmineralization systems of the Yidun arc orogen in Sanjiang region,China.Acta Geologica Sinica,78(1):109-120(in Chinese withEnglish abstract)
Huang XL,Xu YG,Lan JB et al.2009.Neoproterozoic adakitic rocksfrom Mopanshan in the western Yangtze Craton:Partial melts of athickened lower crust.Lithos,112(3-4):367-381
Huang XX,Xu JF,Chen JL et al.2012.Geochronology,geochemistryand petrogenesis of two periods of intermediate-acid intrusive rocksfrom Hongshan area in Zhongdian arc.Acta Petrologica Sinica,28(5):1493-1506(in Chinese with English abstract)
Li JK,Li WC,Wang DH et al.2007.Re-Os dating for ore-forming eventin the late of Yanshan Epoch and research of ore-forming regularity inZhongdian Arc.Acta Petrologica Sinica,23(10):2415-2422(inChinese with English abstract)
Li WC.2007.The tectonic evolution of the Yidun island arc and themetallogenic model of the Pulang porphyry copper deposit,Yunnan,SW China.Ph.D.Dissertation.Beijing:China University ofGeosciences(in Chinese with English summary)
Li WC,Yin GH,Lu YX et al.2009.The evolution and40Ar-39Arisotopic evidence of the Pulang complex in Zhongdian.ActaGeologica Sinica,83(10):1421-1429(in Chinese with Englishabstract)
Li WC,Zeng PS,Hou ZQ et al.2011.The Pulang porphyry copperdeposit and associated felsic intrusions in Yunnan Province,Southwest China.Economic Geologists,105(1):79-92
Li WC,Yin GH,Yu HJ et al.2011.The porphyry metallogenesis ofGeza volcanic magmatic arc in NW Yunnan.Acta Petrologica Sinica,27(9):2541-2552(in Chinese with English abstract)
Lin QC,Xia B and Zhang YQ.2006.Zircon SHRIMP U-Pb dating of thesyn-collisional Xuejiping quartz diorite porphyrite in Zhongdian,Yunnan,China,and its geological implications.Geological Bulletinof China,25(1-2):133-137(in Chinese with English abstract)
Liu XL.2009.Zhongdian island arc magmatic rocks geochemicalcharacteristics and porphyry copper mineralization.Master DegreeThesis.Kunming:Kunming University of Science and Technology(in Chinese with English summary)
Liu YS,Hu ZC,Gao S et al.2008.In situ analysis of major and traceelements of anhydrous minerals by LA-ICP-MS without applying aninternal standard.Chemical Geology,257(1-2):34-43
Liu YS,Gao S,Hu ZC et al.2010.Continental and oceanic crustrecycling-induced melt-peridotite interactions in the Trans-NorthChina Orogen:U-Pb dating,Hf isotopes and trace elements inzircons from mantle xenoliths.Journal of Petrology,51(1-2):537-571
Ludwig KR.2003.User’s Manual for Isoplot3.00:A GeochronologicalToolkit for Microsoft Excel.California:BerkeleyGeochronology Center
Mo XX,Lu FX,Hou ZQ et al.1993.Sanjiang Tethyan Volcanism andRelated Mineralization.Beijing:Geological Publishing House,266-267(in Chinese)
Pan GT,Ding J,Wang LQ et al.2005.The1∶1500000Geological MapSpecification of Qinghai-Tibet Plateau and Its Adjacent Area.3.Chengdu:Chengdu Map Publishing House,266-267(in Chinese)
Pang ZS,Du YS,Wang GW et al.2009.Single-grain zircon U-Pbisotopic ages,geochemistry and its implication of the Pulang complexin Yunnan Province,China.Acta Petrologica Sinica,25(1):159-165(in Chinese with English abstract)
Pearce JA.1983.Role of the sub-continental lithosphere in magmagenesis at active continental margins.In:Hawkesworth CJ and NorryMJ(eds.).Continental Basalts and Mantle Xenoliths.NantwichCheshire:Shiva Publications,230-249
Qu XM and Hou ZQ.2002.40Ar/39Ar age of the Panyong pillow basalt:Implication for the evolution relationship between the Jinshajiang andGarze-Litang suture zones.Geological Review,48(Suppl.):115-121(in Chinese with English abstract)
Reid AJ,Wilson CJL and Liu S.2005.Structural evidence for thePermo-Triassic tectonic evolution of the Yidun Arc,eastern TibetanPlateau.Journal of Structural Geology,27(1):119-137
Reid AJ,Wilson CJL,Liu S et al.2007.Mesozoic plutons of the Yidunarc,SW China:U/Pb geochronology and Hf isotopic signature.OreGeology Review,31(1-4):88-106
Ren JB.2011.The chronology,geochemistry and mineraliziongsignificance of porphyry copper deposits in Zhongdian island arc.Master Degree Thesis.Beijing:Graduate School of Chinese Academyof Sciences(in Chinese with English summary)
Ren JB,Xu JF,Chen JL et al.2011a.Geochemistry and petrogenesis ofPulang porphyries in Sanjiang region.Acta Petrologica etMineralogica,30(4):581-592(in Chinese with English abstract)
Ren JB,Xu JF and Chen JL.2011b.Zircon geochronology and geologicalimplications of ore-bearing porphyries from Zhongdian arc.ActaPetrologica Sinica,27(9):2591-2599(in Chinese with Englishabstract)
Ren T,Zhong H,Chen JF et al.2011.Geochemical characteristics ofthe Langdu high-K intermediate-acid intrusive rocks in the Zhongdianarea,Northwest Yunnan Province,P.R.China.Acta MineralogicaSinica,31(1):43-54(in Chinese with English abstract)
Sun SS and McDonough WF.1989.Chemical and isotopic systematics ofoceanic basalts:Implications for mantle composition and processes.In:Saunders AD and Norry MJ(eds.).Magmatism in OceanicBasins.Geological Society,London,Special Publication,42(1):313-345
Wang BQ,Zhou MF,Li JW et al.2011.Late Triassic porphyriticintrusions and associated volcanic rocks from the Shangri-La region,Yidun terrane,eastern Tibetan Plateau:Adakitic magmatism andporphyry copper mineralization.Lithos,127(1-2):24-38
Wang SX.Zhang XC,Qin CJ et al.2007.Fuild inclusions in quartzveins of Pulang porphyry copper deposit,Zhongdian,northwesternYunnan,China.Geochimica,36(5):467-478(in Chinese withEnglish abstract)
Wang XF,Metcalfe I,Jian P et al.2000.The Jinshajiang-Ailaoshansuture zone,China:Tectonostratigraphy,age and evolution.Journalof Asian Earth Sciences,18(6):675-690
Wang XS,Bi XW,Leng CB et al.2011.LA-ICP-MS zircon U-Pb datingof granite porphyry in the Hongshan Cu-polymetallic deposit,Zhongdian,Northwest Yunnan,China and its geological implication.Acta Mineralogica Sinica,31(3):315-321(in Chinese withEnglish abstract)
Winchester JA and Floyd PA.1977.Geochemical discrimination ofdifferent magma series and their differentiation products usingimmobile elements.Chemical Geology,20:325-343
Wood DA.1980.The application of a Th-Hf-Ta diagram to problems oftectonomagmatic classification and to establishing the nature ofcrustal contamination of basaltic lavas of the British Tertiary VolcanicProvince.Earth and Planetary Science Letters,50(1):11-30
Yang TN,Hou ZQ,Wang Y et al.2012.Late Paleozoic to EarlyMesozoic tectonic evolution of northeast Tibet:Evidence from theTriassic composite western Jinsha-Garzê-Litang suture.Tectonics,31(4):1-20
Yang YQ,Hou ZQ,Huang DA et al.2002.Collision orogenic processand magmatic metallogenic system in Zhongdian arc.ActaGeoscientia Sinica,23(1):17-24(in Chinese with Englishabstract)
Zeng PS,Mo XX,Yu XH et al.2003.Porphyries and porphyry copperdeposits in Zhongdian area,northwestern Yunnan.MineralDeposits,22(4):393-400(in Chinese with English abstract)
Zeng PS,Hou ZQ,Wang HP et al.2004.Re-Os dating of the Pulangporphyry copper deposit in Zhongdian,NW Yunnan,and itsgeological significance.Acta Geologica Sinica,78(2):604-609
Zeng PS,Wang HP,Mo XX et al.2004.Tectonic setting and prospects of porphyry copper deposits in Zhongdian island arc belt.ActaGeoscientica Sinica,25(5):535-540(in Chinese with Englishabstract)
Zeng PS,Li WC,Wang HP et al.2006.The indosinian Pulangsuperlarge porphyry copper deposit in Yunnan,China:Petrology andchronology.Acta Petrologica Sinica,22(4):989-1000(inChinese with English abstract)
Zhang ZM and Jin M.1979.Two kinds of melange and their tectonicsignificance in Xiangcheng-Derong area,southwestern Sichuan.Scientia Geologica Sinica,(3):205-214
曹殿华,王安建,黄玉凤等.2009.中甸弧雪鸡坪斑岩铜矿含矿斑岩锆石SHRIMP U-Pb年代学及Hf同位素组成.地质学报,83(10):1430-1435
陈建林,许继峰,任江波等.2011.俯冲型和碰撞型含矿斑岩地球化学组成的差异.岩石学报,27(9):2733-2742
郭欣,杜杨松,庞振山等.2009.云南普朗斑岩铜矿蚀变带成矿流体特征及其成矿意义.现代地质,23(3):465-471
侯增谦,莫宣学.1991.义敦岛弧的形成演化及其对“三江”地区块状硫化物矿床的控制作用.地球科学,16(2):154-164
侯增谦,曲晓明,周继荣等.2001.三江地区义敦岛弧碰撞造山过程:花岗岩记录.地质学报,75(4):484-497
侯增谦,杨岳清,曲晓明等.2004.三江地区义敦岛弧造山带演化和成矿系统.地质学报,78(1):109-120
黄肖潇,许继峰,陈建林等.2012.中甸岛弧红山地区两期中酸性侵入岩的年代学、地球化学特征及其成因.岩石学报,28(5):1493-1506
李建康,李文昌,王登红等.2007.中甸弧燕山晚期成矿事件的Re-Os定年及成矿规律研究.岩石学报,23(10):2415-2422
李文昌.2007.义敦岛弧构造演化与普朗超大型斑岩铜矿成矿模型.博士学位论文.北京:中国地质大学
李文昌,尹光候,卢映祥等.2009.中甸普朗复式斑岩体演化及40Ar-39Ar同位素依据.地质学报,83(10):1421-1429
李文昌,尹光侯,余海军等.2011.滇西北格咱火山-岩浆弧斑岩成矿作用.岩石学报,27(9):2541-2552
林清茶,夏斌,张玉泉.2006.云南中甸地区雪鸡坪同碰撞石英闪长玢岩锆石SHRIMP U-Pb定年及其意义.地质通报,25(1-2):133-137
刘学龙.2009.中甸岛弧岩浆岩地球化学特征及斑岩型铜矿成矿研究.硕士学位论文.昆明:昆明理工大学
莫宣学,路凤香,侯增谦等.1993.三江特提斯火山作用与成矿.北京:地质出版社,266-267
潘桂堂,丁俊,王立全等.2005.青藏高原及邻区地质图(1∶1500000)说明书.3.成都:成都地图出版社,75-76
庞振山,杜杨松,王功文等.2009.云南普朗复式岩体锆石U-Pb年龄和地球化学特征及其地质意义.岩石学报,25(1):159-165
曲晓明,侯增谦.2002.从潘拥枕状玄武岩的40Ar/39Ar年龄论金沙江缝合带和甘孜-理塘缝合带的演化关系.地质评论,48(增刊):115-121
任江波.2011.中甸岛弧成矿斑岩和矿床的年代学、地球化学研究.硕士学位论文.北京:中国科学院研究生院
任江波,许继峰,陈建林等.2011a.“三江”地区中甸弧普朗成矿斑岩地球化学特征及其成因.岩石矿物学杂志,30(4):581-592
任江波,许继峰,陈建林.2011b.中甸岛弧成矿斑岩的锆石年代学及其意义.岩石学报,27(9):2591-2599
任涛,钟宏,陈金法等.2011.云南中甸地区浪都高钾中酸性侵入岩的地球化学特征.矿物学报,31(1):43-54
王守旭,张兴春,秦朝建等.2007.滇西北中甸普朗斑岩铜矿流体包裹体初步研究.地球化学,36(5):467-478
王新松,毕献武,冷成彪等.2011.滇西北中甸红山Cu多金属矿床花岗斑岩锆石LA-ICP-MS U-Pb定年及其地质意义.矿物学报,31(3):315-321
杨岳清,侯增谦,黄典豪等.2002.中甸弧碰撞造山作用和岩浆成矿系统.地球学报,23(1):12-24
曾普胜,莫宣学,喻学惠等.2003.滇西北中甸斑岩及斑岩铜矿.矿床地质,22(4):393-400
曾普胜,王海平,莫宣学等.2004.中甸岛弧带构造格架及斑岩铜矿前景.地球学报,25(5):535-540
曾普胜,李文昌,王海平等.2006.云南普朗印支期超大型斑岩铜矿床:岩石学及年代学特征.岩石学报,22(4):989-1000
张之孟,金蒙.1979.川西南乡城-得荣地区的两种混杂岩及其构造意义.地质科学,(3):206-214