班公湖—怒江缝合带西段昂龙岗日地区沙木罗组火山岩的岩石大地构造学研究
|
摘要
班公湖—怒江缝合带作为青藏高原的主缝合带之一,其研究对班公湖—怒江特提斯洋的演化和造山带的研究具有重要意义。本文首次对该缝合带西段昂龙岗日地区沙木罗组火山岩进行系统的野外地质调查,并结合全岩地球化学分析,探讨火山岩的成因、构造环境及地球动力学背景。沙木罗组火山岩从底部至顶部共划分出3个火山喷发亚旋回,岩性为安山岩和安山质火山碎屑岩。地球化学分析表明3个亚旋回的火山岩均为钙碱性系列,LREE和不相容元素相对富集,而相对亏损HREE和Nb、P、Ti等高场强元素,具岛弧火山岩的地球化学特征。第一喷发亚旋回火山岩具典型的高镁安山岩特征,暗示是大洋板块俯冲作用的产物,从第一喷发亚旋回至第三喷发亚旋回构造环境由大洋岛弧过渡为大陆边缘弧,火山岩形成于大洋地壳向大陆地壳之下俯冲的背景,且洋壳初始俯冲的时间不晚于晚侏罗世末。岩浆起源于受俯冲板片流体交代的亏损地幔—弱富集地幔,来自俯冲板片的流体上升,引起上覆地幔楔物质发生部分熔融,形成幔源岩浆,在密度差的作用下幔源岩浆向上运移,底侵下地壳,引发下地壳物质发生部分熔融,并与之发生混合作用,形成了研究区火山岩的母岩浆,在岩浆源区或岩浆上升过程中遭受了地壳物质的混染作用,且岩浆演化以部分熔融作用为主,结合区域大地构造背景认为沙木罗组火山岩的形成与班公湖—怒江特提斯洋盆向北向羌塘地块之下俯冲关系密切,沙木罗组角度不整合覆盖在木嘎岗日岩群之上不能作为班公湖—怒江特提斯洋盘闭合的证据。
Objectives: Bangong Lake—Nujiang River Suture Zone is one of the main suture zones in Qinghai—Xizang( Tibet) Plateau,and researches of it have great significance on the researches of the evolutional process of the Tethyan ocean and orogenic belt.Methods: This paper,for the first time,investigates the causes,tectonic settings,and instructions on regional tectonic evolution of volcanic rock by using bulk geochemistry analysis based on systematic field geological investigation of the Shamuluo Formation volcanic rocks in Anglonggangri area located in the west section of the Bangong Lake—Nujiang River Suture Zone.Results: Three volcanic eruption cycles are divided from the top to the bottom with the lithology of andesite and andesitic volcanoclastic rock. Geochemical analysis shows that volcanic rocks in these three cycles belong to calc-alkaline series featured by island arc volcanic rock with relative enrichment of LREE and incompatible element and relative depletion of HREE and high field strength elements like Nb,P,and Ti. Volcanic rocks in the first cycle are featured by classical high-Mg andesite,which implies that plate subduction is likely to start. Tectonic setting from the first eruption cycle to the third one is a transition to continental marginal arc from oceanic island arc. Volcanic rocks in Anglonggangri area are formed during oceanic plate subduction from oceanic crust to the blow of it,and the initial time of subduction is no later than late Jurassic. Source region is depleted—weak enriched mantle influenced by fluid metasomatism of subduction slab. Mantle magma is formed during the partial melting of overriding mantle wedge resulted from ascending fluid of subduction slab,and it migrates upwards as a result of density difference,then intrudes into the lower crust and triggers the partial melting of mantle wedge in the lower crust. Moreover, mantle magma blends with those in the lower crust, thus mother magma of andesite in Anglonggangri area comes into being. Magma source may be contaminated with crustal materials during its ascent process. In addition,magmatic evolution is dominated by partial melting process.Conclusions: Combined with regional tectonic setting,it is considered that the formation of the Shamuluo volcanic rocks is closely correlated with northward subduction of Bangong Lake—Nujiang River's Tethyan oceanic crust beneath the Qiangtang blocks,and the Shamuluo Formation rests with angular unconformity on the Muggar Kangri Group——complex in the area cannot be the evidence for the close of Tethys ocean of Bangong Lake—Nujiang River Suture Zone.
Objectives: Bangong Lake—Nujiang River Suture Zone is one of the main suture zones in Qinghai—Xizang( Tibet) Plateau,and researches of it have great significance on the researches of the evolutional process of the Tethyan ocean and orogenic belt.Methods: This paper,for the first time,investigates the causes,tectonic settings,and instructions on regional tectonic evolution of volcanic rock by using bulk geochemistry analysis based on systematic field geological investigation of the Shamuluo Formation volcanic rocks in Anglonggangri area located in the west section of the Bangong Lake—Nujiang River Suture Zone.Results: Three volcanic eruption cycles are divided from the top to the bottom with the lithology of andesite and andesitic volcanoclastic rock. Geochemical analysis shows that volcanic rocks in these three cycles belong to calc-alkaline series featured by island arc volcanic rock with relative enrichment of LREE and incompatible element and relative depletion of HREE and high field strength elements like Nb,P,and Ti. Volcanic rocks in the first cycle are featured by classical high-Mg andesite,which implies that plate subduction is likely to start. Tectonic setting from the first eruption cycle to the third one is a transition to continental marginal arc from oceanic island arc. Volcanic rocks in Anglonggangri area are formed during oceanic plate subduction from oceanic crust to the blow of it,and the initial time of subduction is no later than late Jurassic. Source region is depleted—weak enriched mantle influenced by fluid metasomatism of subduction slab. Mantle magma is formed during the partial melting of overriding mantle wedge resulted from ascending fluid of subduction slab,and it migrates upwards as a result of density difference,then intrudes into the lower crust and triggers the partial melting of mantle wedge in the lower crust. Moreover, mantle magma blends with those in the lower crust, thus mother magma of andesite in Anglonggangri area comes into being. Magma source may be contaminated with crustal materials during its ascent process. In addition,magmatic evolution is dominated by partial melting process.Conclusions: Combined with regional tectonic setting,it is considered that the formation of the Shamuluo volcanic rocks is closely correlated with northward subduction of Bangong Lake—Nujiang River's Tethyan oceanic crust beneath the Qiangtang blocks,and the Shamuluo Formation rests with angular unconformity on the Muggar Kangri Group——complex in the area cannot be the evidence for the close of Tethys ocean of Bangong Lake—Nujiang River Suture Zone.
引文
陈国荣,刘鸿飞,蒋光武,曾庆高,赵守仁,张相国.2004.西藏班公湖—怒江结合带中段沙木罗组的发现.地质通报,23(2):193 ～ 194.
邓金火,袁振国,杜昌法,唐宗源,孙社良,吕鑫,钟文,万川,钟俊靖.2017.班公湖—怒江结合带西段沙木罗组底砾岩的新发现及地质意义.地质论评,63(2):302 ～ 310.
邓晋福,冯艳芳,狄永军,刘翠,肖庆辉,苏尚国,赵国春,孟斐,马帅,姚图.2015b.岩浆弧火成岩构造组合与洋陆转换.地质论评,61(3):473 ～ 484.
邓晋福,刘翠,冯艳芳,肖庆辉,狄永军,苏尚国,赵国春,段培新,戴蒙.2015a.关于火成岩常用图解的正确使用:讨论与建议.地质论评,61(4):717～ 734.
丁帅,唐菊兴,郑文宝,杨超,张志,王勤,王艺云.2017.西藏拿若斑岩型铜(金) 矿含矿岩体年代学、地球化学及地质意义.地球科学,42(1):1 ～ 23.
杜德道,曲晓明,王根厚,辛洪波,刘治博.2011.西藏班公湖—怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石 U-Pb 年龄和元素地球化学的证据.岩石学报,27(7):1993 ～ 2002.
黄启帅,史仁灯,丁炳华,刘德亮,张晓冉,樊帅权,支霞臣.2012.班公湖MOR型蛇绿岩Re-Os同位素特征对班公湖—怒江特提斯洋裂解时间的制约.岩石矿物学杂志,31(4):465 ～ 478.
雷传扬,李志军,张志,胡正华,王红星,宋俊龙.2012.西藏尕尔穷铜金矿床花岗岩类的地球化学特征及其地球动力学意义.地球学报,33(4):601 ～ 612.
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2018.班公湖—怒江缝合带西段沙木罗组地层中闪长玢岩脉的发现及其地质意义.矿物岩石地球化学通报,37(2):250 ～ 259.
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2019a.班公湖—怒江缝合带西段阿翁错地区中酸性侵入岩的成因及其对区域构造演化的指示.大地构造与成矿学,43(1):168 ～ 185.
雷传扬,唐菊兴,李威,袁华云,张伟,尹滔,裴亚伦,郎兴海.2019b.班公湖—怒江缝合带西段阿翁错复式岩体的岩浆混合成因:地球化学、年代学和暗色微粒包体证据.岩石学报,35(3):665 ～ 686.
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2019c.藏北阿翁错复式岩体及其暗色微粒包体的年代学、地球化学与地球动力学意义.地质通报,38(4):494 ～ 508.
李华亮,高成,李正汉,张璋,彭智敏,关俊雷.2016.西藏班公湖地区竟柱山组时代及其构造意义.大地构造与成矿学,40(4):663 ～ 673.
廖六根,李晓勇,邹爱建,肖业斌.2006.对藏北嘎色地区沙木罗组的新认识.沉积与特提斯地质,26(2):12 ～ 15.
林彬,唐菊兴,宋扬,王勤,曹华文,Michael Baker,张乐骏,李玉彬.2017.藏北多龙矿集区尕尔勤枕状玄武岩地球化学及SHRIMP测年.地球学报,38(5):702 ～ 710.
刘成军,裴先治,李佐臣,李瑞保,王银川,裴磊,陈有忻,魏方辉,高景民,吴树宽,魏博,胥晓春.2014.秦祁结合部位天水地区磨石沟变基性火山岩错石 U-Pb 年代学、地球化学及其构造意义.地质学报,88(3):347 ～ 360.
曲晓明,王瑞江,辛洪波,赵元艺,樊兴涛.2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学.地球化学,38(6):523 ～ 535.
史仁灯.2005.蛇绿岩研究进展、存在问题及思考.地质论评,51(6):681 ～ 693.
史仁灯.2007.班公湖SSZ型蛇绿岩年龄对班—怒洋时限的制约.科学通报,52(7):936 ～ 941.
史仁灯,黄启帅,刘德亮,樊帅权,张晓冉,丁林,Griffin W L,O’Reilly S Y.2012.古老大陆岩石圈地幔再循环与蛇绿岩中铬铁矿床成因.地质论评,58(4):643 ～ 652.
唐功建,王强.2010.高镁安山岩及其地球动力学意义.岩石学报,26(8):2495 ～ 2512.
陶刚,李智武,朱利东,张玉修,杨文光,陈顺,解龙,杨珍,和源,刘和,李超.2016.羌塘地体南缘改则格列戈阿尔辉长岩锆石 U-Pb 年代学、地球化学及地质意义.地质论评,62(5):1149 ～ 1165.
王明,李才,解超明,吴彦旺,范建军,徐建鑫.2014.藏北羌塘南部冈玛错地区展金组玄武岩的成因及其构造意义.地质通报,33(11):1768 ～ 1777.
王勤,林彬,唐菊兴,宋扬,李彦波,侯俊富,李玉彬,卫鲁杰.2018.多龙矿集区色那东岩体年龄、成因与动力学背景.地球科学,43(4):1125 ～ 1141.
韦少港,宋扬,唐菊兴,高轲,冯军,李彦波,侯淋.2016.西藏色那铜(金) 矿床石英闪长玢岩年代学、地球化学与岩石成因.中国地质,43(6):1894 ～ 1912.
韦少港,唐菊兴,宋扬,刘治博,王勤,林彬,贺文,冯军.2017a.西藏班公湖—怒江缝合带美日切错组中酸性火山岩锆石 U-Pb 年龄、Sr—Nd—Hf 同位素、岩石成因及其构造意义.地质学报,91(1):132 ～ 150.
韦少港,唐菊兴,宋扬,刘治博,王勤,林彬,王艺云,方向,杨欢欢,冯军.2017b.西藏改则多龙矿集区地堡那木岗矿床钾玄质二长花岗斑岩锆石LA-MC-ICP-MS U-Pb 年龄、地球化学特征及其地质意义.地质论评,63(1):189 ～ 206.
夏昭德,姜常义,卢荣辉.2012.新疆阿尔泰东南缘哈拉乔拉镁铁质岩体地球化学特征与地质意义.地球科学,37(5):937 ～ 946.
谢冰晶,程捷,黄传冠.2010.班公湖—怒江结合带西段沙木罗组的发现及意义.东华理工大学学报(自然科学版) ,33(2):159 ～ 164.
张志,方向,唐菊兴,王勤,杨超,王艺云,丁帅,杨欢欢.2017.西藏多龙矿集区尕尔勤斑岩铜矿床年代学及地球化学——兼论硅帽的识别与可能的浅成低温热液矿床.岩石学报,33(2):476 ～ 494.
Atherton M P,Petford N.1993.Generation of sodium—rich magmas from newly underplated basaltic crust.Nature International Weekly Journal of Science,362(6416):144 ～ 146.
Barberi F,Ferrara U,Santacroce R,Treuil M,Varet L.1975.A transitional basalt—pantellerite sequence of fractional crystallization,the Boina center,a far Rift.Ethiopia J.Petrol.,16:22 ～ 56.
Boynton W V.1984.Geochemistry of the rare earth elements:eteorite studies.In:Henderson P.ed.Rare Earth Element Geochemistry.Amsterdam:Elsevier,63 ～ 114.
Chen Guorong,Liu Hongfei,Jiang Guangwu,Zeng Qinggao,Zhao Shouren,Zhang Xiangguo.2004&.Discovery of the Shamuluo Formation in the central segment of the Bangong Co —Nujiang River suture zone,Tibet.Geological Bulletin of China,23(2):193 ～ 194.
Condie K C.2001.Mantle Plumes and Their Record in Earth History.London:Cambridge University Press.
Debari S M.1994.Petrogenesis of the Fiambala gabbroic intrusion,northwestern Argentina,a deep crustal syntectonic pluton in a continental magmatic arc.Journal of Petrology,35(3):679 ～ 713.
Deng Jinhuo,Yuan Zhenguo,Yu Jiang,Du Changfa,Tang Zongyuan,Sun Sheliang,Lu Xin,Zhong Wen,Wan Chuan,Zhong Junjing.2017&.New discovery of the basal conglomerate in the Upper Jurassic—Lower Cretaceous Shamuluo Formation in western part of Bangong Lake—Nujiang River suture zone and its geological significance.Geological Review,63(2):302 ～ 310.
Deng Jinfu,Feng Yanfang,Di Yongjun,Liu Cui,Xiao Qinghui,Su Shangguo,Zhao Guochun,Meng Fei,Ma Shuai,Yao Tu.2015b&.Magmatic arc and ocean—continent transition:discussion.Geological Review,61(3):473 ～ 484.
DengJinfu,Liu Cui,Feng Yanfang,Xiao Qinghui,Di Yongjun,Su Shangguo,Zhao Guochun,Duan Peixin,Dai Meng.2015a&.On the correct application in the common igneous petrological diagrams:discussion and suggestion.Geological Review,61(4):717～ 734.
Ding Shuai,Tang Juxing,Zheng Wenbao,Yang Chao,Zhang Zhi,Wang Qin,Wang Yiyun.2017&.Geochronology and geochemistry of Naruo porphyry Cu(Au) deposit in Duolong ore concentrated area,Tibet,and their geological significance.Earth Science,42(1):1 ～ 23.
Du Dedao,Qu Xiaoming,Wang Genhou,Xin Hongbo,Liu Zhibo.2011&.Bidirectional subduction of the Middle Tethys oceanic basin in the west segment of Bangonghu—Nujiang suture,Tibet:Evidence from zircon U-Pb LA-ICP -MS dating and petrogeochemistry of arc granites.Acta Petrologica Sinica,27(7):1993 ～ 2002.
Hastie A R,Kerr A C,Pearce J A,Mitchell S F.2007.Classification of altered volcanic island arc rocks using immobile trace elements:Development of the Th—Co discrimination diagram.Journal of Petrology,48(12):2341 ～ 2357.
Huang Qishuai,Shi Rendeng,Ding Binghua,Liu Deliang,Zhang Xiaoran,Fan Shuaiquan,Zhi Xiacheng.2012&.Re-Os isotopic evidence of MOR-type ophiolite from the Bangong Co for the opening of Bangong—Nujiang Tethys Ocean.Acta Petrologicaet Mineralogica,31(4):465 ～ 478.
Jahn B M,Wu F Y,Lo C H,Tsai C H.1999.Crust mantle interaction induced by deep subduction of the continental crust:Geochemical and Sr—Nd isotopic evidence from post—collisional mafic—ultramafic intrusions of the northern Dabie complex,central China.Chemical Geology,157:119 ～ 146.
Kamei A,Owada M,Nagao T,Shiraki K.2004.High-Mg diorites derived from Sanukitic HMA magmas,Kyushu Island,Southwest Japan Arc:Evidence from clinopyroxene and whole rock compositions.Lithos,75(3 ～ 4):359 ～ 371.
Kapp P,Murphy M A,Yin A,Harrison T M,Ding L,Guo J H.2003.Mesozoic and cenozoic tectonic evolution of the Shiquanhe area of western Tibet.Tectonics,22(4):253 ～ 253.
Kepezhinskas P K,Defant M J,Drummond M S.1996.Progressive enrichment of island arc mantle by melt—peridotite interaction inferred from Kamchatka xenoliths.Geochimica et Cosmochimica Acta,60:1217 ～ 1229.
Kieffer B,Arndt N,Lapierre H,Astien F,Bosch D,Pecher A and Yirgu G.2004.Flood and shield basalts from Ethiopia:Magmas from the African superswell.Journal of Petrology,45(4):793 ～ 834.
La Flèche MR,Camiré G,Jenner GA.1998.Geochemistry of post Acadian,Carboniferous continental intraplate basalts from the Maritimes Basin,Magdalen islands,Québec,Canada.Chemical Geology,148(3 ～ 4):115 ～ 136.
Lei Chuanyang,Li Zhijun,Zhang Zhi,Hu Zhenghua,Wang Hongxing,Song Junlong.2012&.Geochemical characteristics and geodynamic significance of the granites in the Ga’erqiong Cu—Au deposit,Tibet.Acta Geoscientica Sinica,33(4):601 ～ 612.
Lei Chuanyang,Tang Juxing,Li Wei,Yuan Huayun,Zhang Wei,Yin Tao,Pei Yalun,Lang Xinhai.2019b&.Genesis of magma mixing and mingling of the Awengcuo composite plutons in Western Segment of Bangongco—Nujiang Suture Zone:Evidence from geochemistry,geochronology and mafic microgranular enclaves(MMEs).Acta Petrologica Sinica,35(3):665 ～ 686.
Lei Chuanyang,Wu Jianliang,Yin Xianke,Liu Wen,Wang Bo,Li Wei,Yuan Huayun,Zhang Wei,Yin Tao,Pei Yalun.2019a&.Petrogenesis of intermediate—acid intrusive rocks in Awengcuo area in the west segment of the Bangongco—Nujiang Suture,Tibet,and its instructions to the regional tectonic evolution.Geotectonica et Metallogenia,43(1) :168 ～ 185.
Lei Chuanyang,Wu Jianliang,Yin Xianke,Liu Wen,Wang Bo,Li Wei,Yuan Huayun,Zhang Wei,Yin Tao,Pei Yalun.2019c&.Geochronology,geochemistry and geodynamic significance of Awengcuo composite plutonsand and their dark microgranular enclaves in the North of Tibet,China.Geological Bulletin of China,43(4):494 ～ 50.
Lei Chuanyang,Wu Jianliang,Yin Xianke,Liu Wen,Wang Bo,Li Wei,Yuan Huayun,Zhang Wei,Yin Tao,Pei Yalun.2018&.New discovery of the diorite porphyry vein in the Shamuluo Formation in western segment of Bangong Co—Nujiang suture zone and its geological significance.Bulletin of Mineralogy,Petrology and Geochemistry,37(2):250 ～ 259.
Li Hualiang,Gao Cheng,Li Zhenghan,Zhang Zhang,Peng Zhimin,Guan Junlei.2016&.Age and tectonic significance of Jingzhushan Formation in Bangong Lake area,Tibet.Geotectonica et Metallogenia,40(4):663 ～ 673.
Liao Liugen,Li Xiaoyong,Zou Aijian,XiaoYebin.2006&.New explanation of the Shamuluo Formation in the Gase region,northern Xizang.Sedimentary Geology and Tethyan Geology,26(2):12 ～ 15.
Lin Bin,Tang Juxing,Song Yang,Wang Qin,Cao Huawen,Michael Baker,Zhang Lejun,Li Yubin.2017&.Petrogeochemistry and SHRIMP dating of Ga’erqin pillow basalt in Duolong,Northern Tibet.Acta Geoscientica Sinica,38(5):702 ～ 710.
Liu Chengjun,Pei Xianzhi,Li Zuochen,Li Ruibao,Wang Yinchuan,Pei Lei,Chen Youxin,Wei Fanghui,Gao Jingmin,Wu Shukuan,Wei Bo,Xu Xiaochun.2014&.Moshigou meta—basalt in the Tianshui area in the conjunction of the Qinling—Qilian orogens:Zircon U-Pb geochronology,geochemistry and tectonic implications.Acta Geologica Sinica,88(3):347 ～ 360.
Macdonald R,Rogcrs N W,Fitton J G,Black S,Smith M.2001.Plume—Lithosphere interactions in the generation of the basalts of the Kenya Rift,East Africa.Journal of Petrology,42(5):877 ～ 900.
Maurice A F,Hasta F F,Khiamy A A.2012.Neoproterozoic nascent island arc volcanism from the Nubian Shield of Egypt:Magma genesis and generation of continental crust in intraoceanic arcs.Lithos,(132 ～ 133):1 ～ 20.
McDonough W F,Sun Weidong,Ringwood A E,Jagoutz E,Hofmann A W.1992.Potassium,rubidium,and cesium in the Earth and Moon and the evolution of the mantle of the Earth.Geochimica et Cosmochimica Acta,56(3):1001 ～ 1012.
Pearce J A,Norry M J.1979.Petrogenetic implications of Ti,Zr,Y and Nb varistions in volcanic rock.Contributions to Mineralogy and Petrology,69:33 ～ 47.
Pearce J A,Peate D W.1995.Tectonic implications of the compositor of volcanic arc magmas:Annual reviews.Earth and Planetary Science,23:251 ～ 285.
Pearce J A.1982.Trace element characteristics of lavas from destructive plate boundaries.In:Thorpe R S.Andesie.Chichester:Wiley,525 ～ 548.
Plank T.2005.Constraints from Thorium/Lanthanum on sediment recycling at subduction zones and the evolution of the continents.Journal of Petrology,16(5):921 ～ 944.
Qu Xiaoming,Wang Ruijiang,Xin Hongbo,Zhao Yuanyi,Fan Xingtao.2009&.Geochronology and geochemistry of igneous rocks related to the subduction of the Tethys oceanic plate along the Bangong Lake arc zone,the western Tibetan Plateau.Geochimica,38(6):523 ～ 535.
Saunders A D,Storey M,Kent R W,Norry M J.1992.Consequences of plume—lithosphere interactions.In:Storey B C,Alabaster T and Pankhurst R J(eds.) .Magmatism and the Causes of Continental Breakup.London:Geological Society of London Special Publication,68:41 ～ 60.
Shi Rengdeng,Griffin W L,O'Reilly S Y,Huang Qishuai,Zhang Xiaoran,Liu Deling,Zhi Xiachen,Xia Qiongxia,Ding Ling.2012.Melt—mantle mixing produces podiform chromite deposits in ophiolites:Implications of Re-Os systematics in the Dongqiao Neo—tethyan ophiolite,northern Tibet.Goodwin Research,21(1):194 ～ 206.
Shi Rendeng.2005&.Comment on the Progress in and Probl ems on Ophiol ite Study.Geological Review,51(6):681～ 693.
Shi Rendeng.2007#.SHRIMP dating of the Bangong Lake SSZ-type ophiolite:constraints on the closure time of ocean in the Bangong Lake—Nujiang River,northwestern Tibet.Chinese Science Bulletin,52(7):936 ～ 941.
Shi Rendeng,Huang Qishuai,Liu Deliang,Fan Shuaiquan,Zhang Xiaoran,Dinglin,Griffin W L,O’Reilly S Y.2012&.Recycling of ancient sub—continental lithospheric mantle constraints on the genesis of the ophiolitic podiform chromitites Geological Review,51(6):643 ～ 652.
Smithies R H,Champion D C.2000.The Archaean high-Mg diorite suite:Links to tonalite—trondhjemite—granodiorite magmatism and implications for Early Archaean crustal growth.Journal of Petrology,41(12):1653 ～ 1671.
Spring L,Bussy f,Vannay J C,Hunon S,Cosca M A.1993.Early Permian granitic dykes of alkaline affinity in the Indian High Himalaya of upper Lahul and SE Zanskar:Geochemical characterization and geotectonic implications.Geological Society London Special Publications,74(1):251 ～ 264.
Stampfli G M,Borel G D.2002.A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons.Earth and Planetary Science Letters,196(1 ～ 2):17 ～ 33.
Sun Weidong,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
Tang Gongjian,Wang Qiang.2010&.High-Mg andesites and their geodynamic implications.Acta Petrologica Sinica,26(8):2495 ～ 2512.
Tao Gang,Li Zhiwu,Zhu Lidong,Zhang Yuxiu,Yang Wenguang,Chen Shun,Xie Long,Yang Zhen,He Yuan,Liu He,Li Chao.2016&.LA-ICP-MS zircon U-Pb dating,Geochemistry and tectonicImplications of the Gelegear gabrro at the sourthern edge of Qiangtang terrance,Gaize,Xizang(Tibet) .Geological Review,62(5):1149 ～ 1165.
Tatsumi Y,Hanyu T.2003.Geochemical modeling of dehydration and partial melting of subducting lithosphere:Toward a comprehensive understanding of high-Mg andesite formation in the Setouchi volcanic belt,SW Japan.Geochemistry Geophysics Geosystems,4(9):1081.
Tatsumi Y.2001.Geochemical modeling of partial melting of subducting sediments and subsequent melt—mantle interaction:Generation of high-Mg andesites in the Setouchi volcanic belt,southwest Japan.Geology,29(4):323 ～ 326.
Taylor S R,McLennan S M.1995.The geochemical evolution of the continental crust.Reviews of Geophysics,33(2):241 ～ 265.
Wang Ming,Li Cai,Xie Chaoming,Wu Yanwang,Fan Jianjun,Xu Jianxin.2014&.Petrogenesis of the basalt of Zhanjin Formation in the Gangmar Co area,southern Qiangtang,and its tectonic implications.Geological Bulletin of China,33(11):1768 ～ 1777.
Wang Qin,Lin Bin,Tang Juxing,Song Yang,Li Yanbo,Hou Junfu,LiYubin,Wei Lujie.2018&.Diagenesis,lithogenesis and geodynamic setting of intrusions in Senadong area,Duolong District,Tibet.Earth Science,43(4):1125 ～ 1141.
Weaver B L.1991.The origin of ocean island basalts end-member compositions:Trace element and isotopic constraints.Earth and Planetary Science Letters,104:381 ～ 397.
Wei Shaogang,Song Yang,Tang Juxing,Gao Ke,Feng Jun,Li Yanbo,Hou Lin.2016&.Geochronology,geochemistry and petrogenesis of quartz diorite porphyrite from the Sena copper(gold) deposit,Tibet.Geology in China,43(6):1894 ～ 1912.
Wei Shaogang,Tang Juxing,Song Yang,Liu Zhibo,Wang Qin,Lin Bin,Wang Yiyun,Fang Xiang,Yang Huanhuan,Feng Jun.2017b&.Zircons LA-MC-ICP-MS U-Pb ages,petrochemical,petrological and its significance of the potassic monzonitic granite porphyry from the Duolong ore—concentrated district,Gaize County,Xizang(Tibet) .Geological Review,63(1):189 ～ 206.
Wei Shaogang,Tanu Juxing,Song Yang,Liu Zhibo,Wang Qin,Lin Bin,He Wen,Feng Jun.2017a&.Petrogenesis,zircon U-Pb geochronology and Sr—Nd—Hf isotopes of the intermediate—felsic volcanic rocks from the Duolong deposit in the Bangonghu—Nujiang suture zone,Tibet,and its tectonic significance.Acta Geologica Sinica,91(1):132 ～ 150.
Wilson M.1989.Igneous Petrogenesis.London:Unwin Hyman,1 ～ 466.
Winchester J A,Floyd P A.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20:325 ～ 343.
Woodhead J D,Eggins S M,Johnson R W.1998.Magma genesis in the New Britain Island arc:further insights into melting and mass transfer processes.Journal of Petrology,39(9):1641 ～ 1668.
Xia Zhaode,Jiang Changyi,Lu Ronghui.2012&.Geochemical characteristics and geologic implications of Halaqiaola mafic intrusion,southeast Altai,Xinjiang.Earth Science,37(5):937 ～ 946.
Xie Bingjing,Cheng Jie,Huang Chuanguan.2010&.The found and the significance for the west area of Samut Luo Group in the BanGong Lake—Lu River suture.Journal of East China Institute of Technology,33(2):159 ～ 164.
Zhai Qiangguo,Jahn B M,Su Li,Ernst R E,Wang Kuolung,Zhang Ruyuan,Wang Jun,Tang Suohan.2013.SHRIMP zircon U-Pb geochronology,geochemistry and Sr—Nd—Hf isotopic compositions of a mafic dyke swarm in the Qiangtang terrane,northern Tibet and geodynamic implications.Lithos,174:28 ～ 43.
Zhang Kaijun,Xia Bangdong,Wang Guanmin,Li Yongtie,Ye Hefei.2004.Early Cretaceous stratigraphy,depositional environments,sandstone provenance,and tectonic setting of central Tibet,western China.Geological Society of America Bulletin,116(9):1202 ～ 1222.
Zhang Zhi,Fang Xiang,Tang Juxing,Wang Qin,Yang Chao,Wang Yiyun,Ding Shuai,Yang Huanhuan.2017&.Chronology,geochemical characteristics of the Gaerqin porphyry copper deposit in the Duolong ore concentration area in Tibet and discussion about the identification of the lithoscaps and the possible epithermal deposit.Acta Petrologica Sinica,33(2):476 ～ 494.
Zhu D C,Zhao Z D,Niu Y L,Dilek Y,Wang Q,Ji W H,Dong G C,Sui Q L,Liu Y S,Yuan H L,Mo X X.2012.Cambrian bimodal volcanism in the Lhasa Terrane,southern Tibet:Record of an Early Paleozoic Andean-type magmatic arc in the Australian proto-Tethyan margin.Chemical Geology,328(11):290 ～ 308.
邓金火,袁振国,杜昌法,唐宗源,孙社良,吕鑫,钟文,万川,钟俊靖.2017.班公湖—怒江结合带西段沙木罗组底砾岩的新发现及地质意义.地质论评,63(2):302 ～ 310.
邓晋福,冯艳芳,狄永军,刘翠,肖庆辉,苏尚国,赵国春,孟斐,马帅,姚图.2015b.岩浆弧火成岩构造组合与洋陆转换.地质论评,61(3):473 ～ 484.
邓晋福,刘翠,冯艳芳,肖庆辉,狄永军,苏尚国,赵国春,段培新,戴蒙.2015a.关于火成岩常用图解的正确使用:讨论与建议.地质论评,61(4):717～ 734.
丁帅,唐菊兴,郑文宝,杨超,张志,王勤,王艺云.2017.西藏拿若斑岩型铜(金) 矿含矿岩体年代学、地球化学及地质意义.地球科学,42(1):1 ～ 23.
杜德道,曲晓明,王根厚,辛洪波,刘治博.2011.西藏班公湖—怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石 U-Pb 年龄和元素地球化学的证据.岩石学报,27(7):1993 ～ 2002.
黄启帅,史仁灯,丁炳华,刘德亮,张晓冉,樊帅权,支霞臣.2012.班公湖MOR型蛇绿岩Re-Os同位素特征对班公湖—怒江特提斯洋裂解时间的制约.岩石矿物学杂志,31(4):465 ～ 478.
雷传扬,李志军,张志,胡正华,王红星,宋俊龙.2012.西藏尕尔穷铜金矿床花岗岩类的地球化学特征及其地球动力学意义.地球学报,33(4):601 ～ 612.
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2018.班公湖—怒江缝合带西段沙木罗组地层中闪长玢岩脉的发现及其地质意义.矿物岩石地球化学通报,37(2):250 ～ 259.
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2019a.班公湖—怒江缝合带西段阿翁错地区中酸性侵入岩的成因及其对区域构造演化的指示.大地构造与成矿学,43(1):168 ～ 185.
雷传扬,唐菊兴,李威,袁华云,张伟,尹滔,裴亚伦,郎兴海.2019b.班公湖—怒江缝合带西段阿翁错复式岩体的岩浆混合成因:地球化学、年代学和暗色微粒包体证据.岩石学报,35(3):665 ～ 686.
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2019c.藏北阿翁错复式岩体及其暗色微粒包体的年代学、地球化学与地球动力学意义.地质通报,38(4):494 ～ 508.
李华亮,高成,李正汉,张璋,彭智敏,关俊雷.2016.西藏班公湖地区竟柱山组时代及其构造意义.大地构造与成矿学,40(4):663 ～ 673.
廖六根,李晓勇,邹爱建,肖业斌.2006.对藏北嘎色地区沙木罗组的新认识.沉积与特提斯地质,26(2):12 ～ 15.
林彬,唐菊兴,宋扬,王勤,曹华文,Michael Baker,张乐骏,李玉彬.2017.藏北多龙矿集区尕尔勤枕状玄武岩地球化学及SHRIMP测年.地球学报,38(5):702 ～ 710.
刘成军,裴先治,李佐臣,李瑞保,王银川,裴磊,陈有忻,魏方辉,高景民,吴树宽,魏博,胥晓春.2014.秦祁结合部位天水地区磨石沟变基性火山岩错石 U-Pb 年代学、地球化学及其构造意义.地质学报,88(3):347 ～ 360.
曲晓明,王瑞江,辛洪波,赵元艺,樊兴涛.2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学.地球化学,38(6):523 ～ 535.
史仁灯.2005.蛇绿岩研究进展、存在问题及思考.地质论评,51(6):681 ～ 693.
史仁灯.2007.班公湖SSZ型蛇绿岩年龄对班—怒洋时限的制约.科学通报,52(7):936 ～ 941.
史仁灯,黄启帅,刘德亮,樊帅权,张晓冉,丁林,Griffin W L,O’Reilly S Y.2012.古老大陆岩石圈地幔再循环与蛇绿岩中铬铁矿床成因.地质论评,58(4):643 ～ 652.
唐功建,王强.2010.高镁安山岩及其地球动力学意义.岩石学报,26(8):2495 ～ 2512.
陶刚,李智武,朱利东,张玉修,杨文光,陈顺,解龙,杨珍,和源,刘和,李超.2016.羌塘地体南缘改则格列戈阿尔辉长岩锆石 U-Pb 年代学、地球化学及地质意义.地质论评,62(5):1149 ～ 1165.
王明,李才,解超明,吴彦旺,范建军,徐建鑫.2014.藏北羌塘南部冈玛错地区展金组玄武岩的成因及其构造意义.地质通报,33(11):1768 ～ 1777.
王勤,林彬,唐菊兴,宋扬,李彦波,侯俊富,李玉彬,卫鲁杰.2018.多龙矿集区色那东岩体年龄、成因与动力学背景.地球科学,43(4):1125 ～ 1141.
韦少港,宋扬,唐菊兴,高轲,冯军,李彦波,侯淋.2016.西藏色那铜(金) 矿床石英闪长玢岩年代学、地球化学与岩石成因.中国地质,43(6):1894 ～ 1912.
韦少港,唐菊兴,宋扬,刘治博,王勤,林彬,贺文,冯军.2017a.西藏班公湖—怒江缝合带美日切错组中酸性火山岩锆石 U-Pb 年龄、Sr—Nd—Hf 同位素、岩石成因及其构造意义.地质学报,91(1):132 ～ 150.
韦少港,唐菊兴,宋扬,刘治博,王勤,林彬,王艺云,方向,杨欢欢,冯军.2017b.西藏改则多龙矿集区地堡那木岗矿床钾玄质二长花岗斑岩锆石LA-MC-ICP-MS U-Pb 年龄、地球化学特征及其地质意义.地质论评,63(1):189 ～ 206.
夏昭德,姜常义,卢荣辉.2012.新疆阿尔泰东南缘哈拉乔拉镁铁质岩体地球化学特征与地质意义.地球科学,37(5):937 ～ 946.
谢冰晶,程捷,黄传冠.2010.班公湖—怒江结合带西段沙木罗组的发现及意义.东华理工大学学报(自然科学版) ,33(2):159 ～ 164.
张志,方向,唐菊兴,王勤,杨超,王艺云,丁帅,杨欢欢.2017.西藏多龙矿集区尕尔勤斑岩铜矿床年代学及地球化学——兼论硅帽的识别与可能的浅成低温热液矿床.岩石学报,33(2):476 ～ 494.
Atherton M P,Petford N.1993.Generation of sodium—rich magmas from newly underplated basaltic crust.Nature International Weekly Journal of Science,362(6416):144 ～ 146.
Barberi F,Ferrara U,Santacroce R,Treuil M,Varet L.1975.A transitional basalt—pantellerite sequence of fractional crystallization,the Boina center,a far Rift.Ethiopia J.Petrol.,16:22 ～ 56.
Boynton W V.1984.Geochemistry of the rare earth elements:eteorite studies.In:Henderson P.ed.Rare Earth Element Geochemistry.Amsterdam:Elsevier,63 ～ 114.
Chen Guorong,Liu Hongfei,Jiang Guangwu,Zeng Qinggao,Zhao Shouren,Zhang Xiangguo.2004&.Discovery of the Shamuluo Formation in the central segment of the Bangong Co —Nujiang River suture zone,Tibet.Geological Bulletin of China,23(2):193 ～ 194.
Condie K C.2001.Mantle Plumes and Their Record in Earth History.London:Cambridge University Press.
Debari S M.1994.Petrogenesis of the Fiambala gabbroic intrusion,northwestern Argentina,a deep crustal syntectonic pluton in a continental magmatic arc.Journal of Petrology,35(3):679 ～ 713.
Deng Jinhuo,Yuan Zhenguo,Yu Jiang,Du Changfa,Tang Zongyuan,Sun Sheliang,Lu Xin,Zhong Wen,Wan Chuan,Zhong Junjing.2017&.New discovery of the basal conglomerate in the Upper Jurassic—Lower Cretaceous Shamuluo Formation in western part of Bangong Lake—Nujiang River suture zone and its geological significance.Geological Review,63(2):302 ～ 310.
Deng Jinfu,Feng Yanfang,Di Yongjun,Liu Cui,Xiao Qinghui,Su Shangguo,Zhao Guochun,Meng Fei,Ma Shuai,Yao Tu.2015b&.Magmatic arc and ocean—continent transition:discussion.Geological Review,61(3):473 ～ 484.
DengJinfu,Liu Cui,Feng Yanfang,Xiao Qinghui,Di Yongjun,Su Shangguo,Zhao Guochun,Duan Peixin,Dai Meng.2015a&.On the correct application in the common igneous petrological diagrams:discussion and suggestion.Geological Review,61(4):717～ 734.
Ding Shuai,Tang Juxing,Zheng Wenbao,Yang Chao,Zhang Zhi,Wang Qin,Wang Yiyun.2017&.Geochronology and geochemistry of Naruo porphyry Cu(Au) deposit in Duolong ore concentrated area,Tibet,and their geological significance.Earth Science,42(1):1 ～ 23.
Du Dedao,Qu Xiaoming,Wang Genhou,Xin Hongbo,Liu Zhibo.2011&.Bidirectional subduction of the Middle Tethys oceanic basin in the west segment of Bangonghu—Nujiang suture,Tibet:Evidence from zircon U-Pb LA-ICP -MS dating and petrogeochemistry of arc granites.Acta Petrologica Sinica,27(7):1993 ～ 2002.
Hastie A R,Kerr A C,Pearce J A,Mitchell S F.2007.Classification of altered volcanic island arc rocks using immobile trace elements:Development of the Th—Co discrimination diagram.Journal of Petrology,48(12):2341 ～ 2357.
Huang Qishuai,Shi Rendeng,Ding Binghua,Liu Deliang,Zhang Xiaoran,Fan Shuaiquan,Zhi Xiacheng.2012&.Re-Os isotopic evidence of MOR-type ophiolite from the Bangong Co for the opening of Bangong—Nujiang Tethys Ocean.Acta Petrologicaet Mineralogica,31(4):465 ～ 478.
Jahn B M,Wu F Y,Lo C H,Tsai C H.1999.Crust mantle interaction induced by deep subduction of the continental crust:Geochemical and Sr—Nd isotopic evidence from post—collisional mafic—ultramafic intrusions of the northern Dabie complex,central China.Chemical Geology,157:119 ～ 146.
Kamei A,Owada M,Nagao T,Shiraki K.2004.High-Mg diorites derived from Sanukitic HMA magmas,Kyushu Island,Southwest Japan Arc:Evidence from clinopyroxene and whole rock compositions.Lithos,75(3 ～ 4):359 ～ 371.
Kapp P,Murphy M A,Yin A,Harrison T M,Ding L,Guo J H.2003.Mesozoic and cenozoic tectonic evolution of the Shiquanhe area of western Tibet.Tectonics,22(4):253 ～ 253.
Kepezhinskas P K,Defant M J,Drummond M S.1996.Progressive enrichment of island arc mantle by melt—peridotite interaction inferred from Kamchatka xenoliths.Geochimica et Cosmochimica Acta,60:1217 ～ 1229.
Kieffer B,Arndt N,Lapierre H,Astien F,Bosch D,Pecher A and Yirgu G.2004.Flood and shield basalts from Ethiopia:Magmas from the African superswell.Journal of Petrology,45(4):793 ～ 834.
La Flèche MR,Camiré G,Jenner GA.1998.Geochemistry of post Acadian,Carboniferous continental intraplate basalts from the Maritimes Basin,Magdalen islands,Québec,Canada.Chemical Geology,148(3 ～ 4):115 ～ 136.
Lei Chuanyang,Li Zhijun,Zhang Zhi,Hu Zhenghua,Wang Hongxing,Song Junlong.2012&.Geochemical characteristics and geodynamic significance of the granites in the Ga’erqiong Cu—Au deposit,Tibet.Acta Geoscientica Sinica,33(4):601 ～ 612.
Lei Chuanyang,Tang Juxing,Li Wei,Yuan Huayun,Zhang Wei,Yin Tao,Pei Yalun,Lang Xinhai.2019b&.Genesis of magma mixing and mingling of the Awengcuo composite plutons in Western Segment of Bangongco—Nujiang Suture Zone:Evidence from geochemistry,geochronology and mafic microgranular enclaves(MMEs).Acta Petrologica Sinica,35(3):665 ～ 686.
Lei Chuanyang,Wu Jianliang,Yin Xianke,Liu Wen,Wang Bo,Li Wei,Yuan Huayun,Zhang Wei,Yin Tao,Pei Yalun.2019a&.Petrogenesis of intermediate—acid intrusive rocks in Awengcuo area in the west segment of the Bangongco—Nujiang Suture,Tibet,and its instructions to the regional tectonic evolution.Geotectonica et Metallogenia,43(1) :168 ～ 185.
Lei Chuanyang,Wu Jianliang,Yin Xianke,Liu Wen,Wang Bo,Li Wei,Yuan Huayun,Zhang Wei,Yin Tao,Pei Yalun.2019c&.Geochronology,geochemistry and geodynamic significance of Awengcuo composite plutonsand and their dark microgranular enclaves in the North of Tibet,China.Geological Bulletin of China,43(4):494 ～ 50.
Lei Chuanyang,Wu Jianliang,Yin Xianke,Liu Wen,Wang Bo,Li Wei,Yuan Huayun,Zhang Wei,Yin Tao,Pei Yalun.2018&.New discovery of the diorite porphyry vein in the Shamuluo Formation in western segment of Bangong Co—Nujiang suture zone and its geological significance.Bulletin of Mineralogy,Petrology and Geochemistry,37(2):250 ～ 259.
Li Hualiang,Gao Cheng,Li Zhenghan,Zhang Zhang,Peng Zhimin,Guan Junlei.2016&.Age and tectonic significance of Jingzhushan Formation in Bangong Lake area,Tibet.Geotectonica et Metallogenia,40(4):663 ～ 673.
Liao Liugen,Li Xiaoyong,Zou Aijian,XiaoYebin.2006&.New explanation of the Shamuluo Formation in the Gase region,northern Xizang.Sedimentary Geology and Tethyan Geology,26(2):12 ～ 15.
Lin Bin,Tang Juxing,Song Yang,Wang Qin,Cao Huawen,Michael Baker,Zhang Lejun,Li Yubin.2017&.Petrogeochemistry and SHRIMP dating of Ga’erqin pillow basalt in Duolong,Northern Tibet.Acta Geoscientica Sinica,38(5):702 ～ 710.
Liu Chengjun,Pei Xianzhi,Li Zuochen,Li Ruibao,Wang Yinchuan,Pei Lei,Chen Youxin,Wei Fanghui,Gao Jingmin,Wu Shukuan,Wei Bo,Xu Xiaochun.2014&.Moshigou meta—basalt in the Tianshui area in the conjunction of the Qinling—Qilian orogens:Zircon U-Pb geochronology,geochemistry and tectonic implications.Acta Geologica Sinica,88(3):347 ～ 360.
Macdonald R,Rogcrs N W,Fitton J G,Black S,Smith M.2001.Plume—Lithosphere interactions in the generation of the basalts of the Kenya Rift,East Africa.Journal of Petrology,42(5):877 ～ 900.
Maurice A F,Hasta F F,Khiamy A A.2012.Neoproterozoic nascent island arc volcanism from the Nubian Shield of Egypt:Magma genesis and generation of continental crust in intraoceanic arcs.Lithos,(132 ～ 133):1 ～ 20.
McDonough W F,Sun Weidong,Ringwood A E,Jagoutz E,Hofmann A W.1992.Potassium,rubidium,and cesium in the Earth and Moon and the evolution of the mantle of the Earth.Geochimica et Cosmochimica Acta,56(3):1001 ～ 1012.
Pearce J A,Norry M J.1979.Petrogenetic implications of Ti,Zr,Y and Nb varistions in volcanic rock.Contributions to Mineralogy and Petrology,69:33 ～ 47.
Pearce J A,Peate D W.1995.Tectonic implications of the compositor of volcanic arc magmas:Annual reviews.Earth and Planetary Science,23:251 ～ 285.
Pearce J A.1982.Trace element characteristics of lavas from destructive plate boundaries.In:Thorpe R S.Andesie.Chichester:Wiley,525 ～ 548.
Plank T.2005.Constraints from Thorium/Lanthanum on sediment recycling at subduction zones and the evolution of the continents.Journal of Petrology,16(5):921 ～ 944.
Qu Xiaoming,Wang Ruijiang,Xin Hongbo,Zhao Yuanyi,Fan Xingtao.2009&.Geochronology and geochemistry of igneous rocks related to the subduction of the Tethys oceanic plate along the Bangong Lake arc zone,the western Tibetan Plateau.Geochimica,38(6):523 ～ 535.
Saunders A D,Storey M,Kent R W,Norry M J.1992.Consequences of plume—lithosphere interactions.In:Storey B C,Alabaster T and Pankhurst R J(eds.) .Magmatism and the Causes of Continental Breakup.London:Geological Society of London Special Publication,68:41 ～ 60.
Shi Rengdeng,Griffin W L,O'Reilly S Y,Huang Qishuai,Zhang Xiaoran,Liu Deling,Zhi Xiachen,Xia Qiongxia,Ding Ling.2012.Melt—mantle mixing produces podiform chromite deposits in ophiolites:Implications of Re-Os systematics in the Dongqiao Neo—tethyan ophiolite,northern Tibet.Goodwin Research,21(1):194 ～ 206.
Shi Rendeng.2005&.Comment on the Progress in and Probl ems on Ophiol ite Study.Geological Review,51(6):681～ 693.
Shi Rendeng.2007#.SHRIMP dating of the Bangong Lake SSZ-type ophiolite:constraints on the closure time of ocean in the Bangong Lake—Nujiang River,northwestern Tibet.Chinese Science Bulletin,52(7):936 ～ 941.
Shi Rendeng,Huang Qishuai,Liu Deliang,Fan Shuaiquan,Zhang Xiaoran,Dinglin,Griffin W L,O’Reilly S Y.2012&.Recycling of ancient sub—continental lithospheric mantle constraints on the genesis of the ophiolitic podiform chromitites Geological Review,51(6):643 ～ 652.
Smithies R H,Champion D C.2000.The Archaean high-Mg diorite suite:Links to tonalite—trondhjemite—granodiorite magmatism and implications for Early Archaean crustal growth.Journal of Petrology,41(12):1653 ～ 1671.
Spring L,Bussy f,Vannay J C,Hunon S,Cosca M A.1993.Early Permian granitic dykes of alkaline affinity in the Indian High Himalaya of upper Lahul and SE Zanskar:Geochemical characterization and geotectonic implications.Geological Society London Special Publications,74(1):251 ～ 264.
Stampfli G M,Borel G D.2002.A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons.Earth and Planetary Science Letters,196(1 ～ 2):17 ～ 33.
Sun Weidong,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
Tang Gongjian,Wang Qiang.2010&.High-Mg andesites and their geodynamic implications.Acta Petrologica Sinica,26(8):2495 ～ 2512.
Tao Gang,Li Zhiwu,Zhu Lidong,Zhang Yuxiu,Yang Wenguang,Chen Shun,Xie Long,Yang Zhen,He Yuan,Liu He,Li Chao.2016&.LA-ICP-MS zircon U-Pb dating,Geochemistry and tectonicImplications of the Gelegear gabrro at the sourthern edge of Qiangtang terrance,Gaize,Xizang(Tibet) .Geological Review,62(5):1149 ～ 1165.
Tatsumi Y,Hanyu T.2003.Geochemical modeling of dehydration and partial melting of subducting lithosphere:Toward a comprehensive understanding of high-Mg andesite formation in the Setouchi volcanic belt,SW Japan.Geochemistry Geophysics Geosystems,4(9):1081.
Tatsumi Y.2001.Geochemical modeling of partial melting of subducting sediments and subsequent melt—mantle interaction:Generation of high-Mg andesites in the Setouchi volcanic belt,southwest Japan.Geology,29(4):323 ～ 326.
Taylor S R,McLennan S M.1995.The geochemical evolution of the continental crust.Reviews of Geophysics,33(2):241 ～ 265.
Wang Ming,Li Cai,Xie Chaoming,Wu Yanwang,Fan Jianjun,Xu Jianxin.2014&.Petrogenesis of the basalt of Zhanjin Formation in the Gangmar Co area,southern Qiangtang,and its tectonic implications.Geological Bulletin of China,33(11):1768 ～ 1777.
Wang Qin,Lin Bin,Tang Juxing,Song Yang,Li Yanbo,Hou Junfu,LiYubin,Wei Lujie.2018&.Diagenesis,lithogenesis and geodynamic setting of intrusions in Senadong area,Duolong District,Tibet.Earth Science,43(4):1125 ～ 1141.
Weaver B L.1991.The origin of ocean island basalts end-member compositions:Trace element and isotopic constraints.Earth and Planetary Science Letters,104:381 ～ 397.
Wei Shaogang,Song Yang,Tang Juxing,Gao Ke,Feng Jun,Li Yanbo,Hou Lin.2016&.Geochronology,geochemistry and petrogenesis of quartz diorite porphyrite from the Sena copper(gold) deposit,Tibet.Geology in China,43(6):1894 ～ 1912.
Wei Shaogang,Tang Juxing,Song Yang,Liu Zhibo,Wang Qin,Lin Bin,Wang Yiyun,Fang Xiang,Yang Huanhuan,Feng Jun.2017b&.Zircons LA-MC-ICP-MS U-Pb ages,petrochemical,petrological and its significance of the potassic monzonitic granite porphyry from the Duolong ore—concentrated district,Gaize County,Xizang(Tibet) .Geological Review,63(1):189 ～ 206.
Wei Shaogang,Tanu Juxing,Song Yang,Liu Zhibo,Wang Qin,Lin Bin,He Wen,Feng Jun.2017a&.Petrogenesis,zircon U-Pb geochronology and Sr—Nd—Hf isotopes of the intermediate—felsic volcanic rocks from the Duolong deposit in the Bangonghu—Nujiang suture zone,Tibet,and its tectonic significance.Acta Geologica Sinica,91(1):132 ～ 150.
Wilson M.1989.Igneous Petrogenesis.London:Unwin Hyman,1 ～ 466.
Winchester J A,Floyd P A.1977.Geochemical discrimination of different magma series and their differentiation products using immobile elements.Chemical Geology,20:325 ～ 343.
Woodhead J D,Eggins S M,Johnson R W.1998.Magma genesis in the New Britain Island arc:further insights into melting and mass transfer processes.Journal of Petrology,39(9):1641 ～ 1668.
Xia Zhaode,Jiang Changyi,Lu Ronghui.2012&.Geochemical characteristics and geologic implications of Halaqiaola mafic intrusion,southeast Altai,Xinjiang.Earth Science,37(5):937 ～ 946.
Xie Bingjing,Cheng Jie,Huang Chuanguan.2010&.The found and the significance for the west area of Samut Luo Group in the BanGong Lake—Lu River suture.Journal of East China Institute of Technology,33(2):159 ～ 164.
Zhai Qiangguo,Jahn B M,Su Li,Ernst R E,Wang Kuolung,Zhang Ruyuan,Wang Jun,Tang Suohan.2013.SHRIMP zircon U-Pb geochronology,geochemistry and Sr—Nd—Hf isotopic compositions of a mafic dyke swarm in the Qiangtang terrane,northern Tibet and geodynamic implications.Lithos,174:28 ～ 43.
Zhang Kaijun,Xia Bangdong,Wang Guanmin,Li Yongtie,Ye Hefei.2004.Early Cretaceous stratigraphy,depositional environments,sandstone provenance,and tectonic setting of central Tibet,western China.Geological Society of America Bulletin,116(9):1202 ～ 1222.
Zhang Zhi,Fang Xiang,Tang Juxing,Wang Qin,Yang Chao,Wang Yiyun,Ding Shuai,Yang Huanhuan.2017&.Chronology,geochemical characteristics of the Gaerqin porphyry copper deposit in the Duolong ore concentration area in Tibet and discussion about the identification of the lithoscaps and the possible epithermal deposit.Acta Petrologica Sinica,33(2):476 ～ 494.
Zhu D C,Zhao Z D,Niu Y L,Dilek Y,Wang Q,Ji W H,Dong G C,Sui Q L,Liu Y S,Yuan H L,Mo X X.2012.Cambrian bimodal volcanism in the Lhasa Terrane,southern Tibet:Record of an Early Paleozoic Andean-type magmatic arc in the Australian proto-Tethyan margin.Chemical Geology,328(11):290 ～ 308.