[1] |
潘桂棠,郑海翔,徐跃荣,等.初论班公湖-怒江结合带[C]//青藏高原地质文集,1983(4):229-242.
Google Scholar
|
[2] |
潘桂棠.东特提斯地质构造形成演化[M].北京:地质出版社,1997.
Google Scholar
|
[3] |
潘桂棠,李兴振,王立全,等.青藏高原及邻区大地构造单元初步划分[J].地质通报,2002,21(11):701-707.
Google Scholar
|
[4] |
李才.龙木错-双湖-澜沧江板块缝合带与石炭-二叠纪冈瓦纳北界[J].长春地质学院学报,1987,17(2):155-166.
Google Scholar
|
[5] |
Yin A,Harrison T M.Geologic Evolution of the Himalayan-Tibetan Orogen[J].Annual Review of Earth&Planetary Sciences,2000,28(1):211-280.
Google Scholar
|
[6] |
Qiu R Z,Zhou S,Deng J F,et al.Dating of gabbro in the Shemalagouophiolite in the westernsegment of the Bangong Co-Nujiangophiolite belt,Tibet-with a discussion of the age of the Bangong Co-Nujiangophiolite belt[J].Chinese Geology,2004,31(3):262-268.
Google Scholar
|
[7] |
潘桂棠,莫宣学,侯增谦,等.冈底斯造山带的时空结构及演化[J].岩石学报,2006,22(3):521-533.
Google Scholar
|
[8] |
段志明,李光明,张晖,等.色那金矿石英二长闪长岩锆石U-Pb年龄与地球化学特征及其对成矿背景的约束[J].吉林大学学报,2013,43(6):1865-1877.
Google Scholar
|
[9] |
李金祥,李光明,秦克章,等.班公湖带多不杂富金斑岩铜矿床斑岩-火山岩的地球化学特征与时代对成矿构造背景的制约[J].岩石学报,2008,24(3):531-543.
Google Scholar
|
[10] |
潘桂棠,朱弟成,王立权,等.班公湖-怒江缝合带作为冈瓦纳大陆北界的地质地球物理证据[J].地学前缘,2004,11(4):371-382.
Google Scholar
|
[11] |
李光明,段志明,刘波,等.西藏班公湖-怒江缝合带北缘多龙地区侏罗纪增生杂岩的特征及意义[J].地质通报,2003,22(8):1256-1260.
Google Scholar
|
[12] |
朱弟成,潘桂棠,莫宣学,等.青藏高原中部中生代OIB型玄武岩的识别:年代学、地球化学及其构造环境[J].地质通报,2006,25(9):1312-1328.
Google Scholar
|
[13] |
Kapp P,Murphy M A,Yin A,et al.Mesozoic and Cenozoic tectonic evolution of the Shiquanhe area of western Tibet[J].Tectonics,2003,22(4):253-253.
Google Scholar
|
[14] |
Zhu D C,Mo X X,Niu Y L,et al.Geochemical investigation of Early Cretaceous igneous rocks along an east-west traverse throughout the central Lhasa Terrane,Tibet[J].Chemical Geology,2009,268:298-312.
Google Scholar
|
[15] |
曲晓明,辛洪波.藏西班公湖斑岩铜矿带的形成时代与成矿构造环境[J].地质通报,2006,25(7):792-799.
Google Scholar
|
[16] |
Shi R D.SHRIMP dating of the Bangong Lake SSZ-type ophiolite:Constraints on the closure time of theocean in the Bangong Lake-Nujiang River,northwestern Tibet[J].Chinese Science Bulletin,2007,52(7):936-941.
Google Scholar
|
[17] |
张玉修.班公湖-怒江缝合带中西段构造演化[D].中国科学院广州地球化学研究所博士学位论文.2007.
Google Scholar
|
[18] |
Chen Y,Zhu D C,Zhao Z D,et al.Slab breakoff triggered ca.113 Ma magmatism around Xainza area of the Lhasa Terrane,Tibet[J].Gondwana Research,2014,26:449-463.
Google Scholar
|
[19] |
Xu M J,Li C,Xu W,et al.Petrology,Geochemistry and Geochronology of Gabbros from the ZhongcangOphiolitic Mélange,Central Tibet:Implications for an Intra-Oceanic Subduction Zone within the Neo-Tethys Ocean[J].Journal of Earth Science,2014,25(2):224-240.
Google Scholar
|
[20] |
Fan J J,Li C,Xie C M,et al.Petrology,geochemistry,and geochronology of the zhonggang ocean island,gaize county,northern Tibet:implications for the evolution of the Bangongco-Nujiang ocean[J].International Geology Review,2014,56:1504-1520.
Google Scholar
|
[21] |
Fan J J,Li C,Xie C M,et al.Petrology and U-Pb zircon geochronology of bimdal volcanic rocks from the Maierze Group,northern Tibet:Constraints on the timing of closure of the Bangong-Nujiang Ocean[J].Lithos,2015,277:148-160.
Google Scholar
|
[22] |
Liu D L,Huang Q S,Fan S Q,et al.Subduction of the Bangong-Nujiang Ocean:constraints from granites in the Bangong Co area,Tibet[J].Geological Journal,2014,49:188-206.
Google Scholar
|
[23] |
陈华安,朱向平,马东方,等.西藏波龙斑岩铜金矿床成矿斑岩年代学、岩石化学特征及其成矿意义[J].地质学报,2013,87(10):1593-1611.
Google Scholar
|
[24] |
李兴奎,李才,孙振明,等.西藏赛角铜金矿闪长岩LA-ICP-MS锆石U-Pb年龄、Hf同位素和地球化学特征及成矿意义[J].地质通报,2015,34(5):908-918.
Google Scholar
|
[25] |
Zhu D C,Li S M,Cawood P A,et al.Assembly of the Lhasa and Qiangtangterranes in central Tibet by divergent double subduction[J].Lithos,2015,245:7-17.
Google Scholar
|
[26] |
何阳阳,温春齐,等.西藏多不杂铜矿区曲色组砂岩化学组分特征及构造背景[J].成都理工大学学报(自然科学版),2014,41(1):113-118.
Google Scholar
|
[27] |
段志明,李光明,张晖,等.西藏班公湖-怒江缝合带北缘多龙矿集区晚三叠世-侏罗纪增生杂岩结构及其对成矿地质背景的约束[J].地质通报,2013,32(5):743-750.
Google Scholar
|
[28] |
Li J,Qin K,Li G,et al.Magmatic-hydrothermal evolution of the Cretaceous Duolong gold-rich porphyry copper deposit in the Bangongcometallogenic belt,Tibet:Evidence from U-Pb and 40Ar/39Ar geochronology[J].Journal of Asian Earth Sciences,2011,41(6):525-536.
Google Scholar
|
[29] |
Li J X,Qin K Z,Li G M,et al.Geochronology,geochemistry,and zircon Hf isotopic compositions of Mesozoic intermediate-felsic intrusions in central Tibet:Petrogenetic and tectonic implications[J].Lithos,2014,198(1):77-91.
Google Scholar
|
[30] |
Xu W,Li C,Wang M,et al.Subduction of a spreading ridge within the Bangong Co-Nujiang Tethys Ocean:Evidence from Early Cretaceous mafic dykes in the Duolong porphyry Cu-Au deposit,western Tibet[J].Gondwana Research,2015,doi:10.1016/j.gr.2015.09.010.
Google Scholar
|
[31] |
辛洪波,曲晓明,王瑞江,等.藏西班公湖斑岩铜矿带成矿斑岩地球化学及Pb、Sr、Nd同位素特征[J].矿床地质,2009,28(6):785-792.
Google Scholar
|
[32] |
Yuan H,Gao S,Liu X,et al.Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry[J].Geostandards&Geoanalytical Research,2004,28(3):353-370.
Google Scholar
|
[33] |
李长民.锆石成因矿物学与锆石微区定年综述[J].地质调查与研究,2009,33(3):161-174.
Google Scholar
|
[34] |
刘世坤,吕荣敬.羌塘地区海相下侏罗统新知[J].地层学杂志,1988,12(2):133-135.
Google Scholar
|
[35] |
佘宏全,李进文,马东方,等.西藏多不杂斑岩铜矿床辉钼矿Re-Os和锆石U-Pb SHRIMP测年及地质意义[J].矿床地质,2009,28(6):737-746.
Google Scholar
|
[36] |
吕立娜.西藏班公湖-怒江成矿带西段富铁与铜(金)矿床模型[D].中国地质科学院博士学位论文,2012.
Google Scholar
|
[37] |
符家骏,赵元艺,郭硕.西藏多龙矿集区花岗闪长斑岩地球化学特征及其意义[J].岩石矿物学杂志,2014,33(6):1039-1051.
Google Scholar
|
[38] |
常青松,朱弟成,赵志丹,等.西藏羌塘南缘热那错早白垩世流纹岩锆石U-Pb年代学和Hf同位素及其意义[J].岩石学报,2011,27(7):2034-2044.
Google Scholar
|
[39] |
祝向平,陈华安,马东方,等.西藏波龙斑岩铜金矿床的Re-Os同位素年龄及其地质意义[J].岩石学报,2011,27(7):2159-2164.
Google Scholar
|