Williams H,Turner S,Kelley S and Harris N.2001.Age and composition of dikes in Southern Tibet:New constraints on the timing of east-west extension and its relationship to postcollisional volcanism.Geology,29:339～342.
[2]
Wilson M.1989.Igneous Petrogenesis:A global tectonic approach.London:Unwin Hyman,1～466.
[3]
Woodhead J D and McCulloch M T.1989.Ancient seafloor signals in Pitcairn Island lavas and evidenc for large amplitude,small lengthscale mantle heterogeneities.Earth Planetary Sci.Lett.,94(3):257～273.
[4]
Xie Guiqing,Hu Ruizhong and Jia Dacheng.2002.Geological and geochemical characteristics and its significance of mafic dikes from Northwest Jiangxi Province.Geochimica,31 (4):329～ 337 (in Chinese with English abstract).
[5]
Yang Jinhui,Chung Sunlin,Zhai Mingguo and Zhou Xinhua.2004.Geochemical and Sr-Nd-Pb isotopic compositions of mafic dikes from the Jaodong Peninsula,China:evidence for vein-plusperidotite melting in the lithospheric mantle.Lithos,73:145～160.
[6]
Zeng Wen,Zhong Zengqiu,Zhou Hanwen,Jiang Linsheng,Zhou Zhongyou and Chen Tielong.2004.Geochemistry of mafic dykes in Huangling area and its tectonic implications.Earth ScienceJournal of China University of Geosciences,29 (1):31 ～ 38 (in Chinese with English abstract).
[7]
Zhang Guishan,Wen Hanjie and Qiu Yuzhuo.2004.Geochemistry of the late Mesozoic mafic dikes in western Fujian Province.Geochimica,33 (3):243 ～ 253 (in Chinese with English abstract).
[8]
Zhao Zhenghua,Bao Zhiwei and Zhang Baiyou.1998.Geochemical characteristics of the Mesozoic basalts from south Hunan Province.Science in China (Series D),28 (supp.):7 ～ 14 (in Chinese).
[9]
Zhong Huaming,Xia Jun,Tong Jinsong,Lu Rukui,Li Yunhuai and Xu Shengfa,2004.New results and major progress in regional geological survky of the Lhozag County Sheet.Geological Bulletin of China,23(5-6):451～457 (in Chinese with English abstract).
Alpaslan M,Frei R,Boztug D,Kurt M A and Temel A.2004.Geochemical and Pb-Sr-Nd isotopic constraints indicating an enriched-mantle source for late Cretaceous to early Tertiary volcanism,central Anatolia,Turkey.International Geology Review,46:1022～ 1041.
[25]
Burchfiel,B.C.,Chen,Z,Hodges,K.V.,Liu,Y.,Royden,L.H.,Deng,C.and Xu,J.,1992.The South Tibetan Detachment System,Himalayan orogen:Extension contemporaneous with and parallel to shortening in a collisional mountain belt.Geological Society of America,Special Paper,269:1～51.
[26]
Gao Yongfeng,Hou Zengqian,Wei Ruihua,Cai Jianghui,Meng Xiangjin and Huang Wei.2003.Origin of a basic -ultrabasic belt on the northern bank of the Yarlung Zangbo River.Geological Bulletin of China,22(10):789～797 (in Chinese with English abstract).
[27]
Guillot S,Le Fort P.1995.Geochemical constraints on the bimodal origin of High Himalayan leucogranite.Lithos,35:221～234.
[28]
Halama R,Marks M,Brügmann G,Siebel W,Wenzel T and Markl G.2004.Crustal contamination of mafic magmas:evidence from a petrological,geochemical and Sr-Nd-Os-O isotope study of the Proterozoic Isortoq dike swarm,South Greenland.Lithos,74:199～232.
[29]
Harrison T M,McKeegan K D,Le Fort P.1995.Detection of Inherited monazite in the Manaslu leucogranite by 208Pb/232Th ion microprobe dating:Crystallization age and tectonic significance.Earth and Planetary Science Letters,133:271 ～282.
[30]
Hofmann A W.1997.Mantle geochemistry:the message from oceanic volcanism.Nature,385:219～229.
[31]
Hou ZQ,Gao YF,Meng XJ,Qu XM and Huang W.2004.Genesis of adakitic 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).
[32]
Jagoutz E,Palme H,Baddenhausen H,Blum K,Cendales M,Dreibus G,Spottel B,Lorenz V and Wanke H.1979.The abundances of major,minor and trace elements in the earth\'s mantle as derived from primitive ultramafic nodules.Proc.Lunar.and Planet.Sci.Conf.No.10,Geochim.Cosmochim.Acta,Supplement 11,2031～2050.
[33]
Jiang Sihong,Nie Fengjun.2003.Nd-isotope constraints on origin of the Shuiquangou intrusive complex,north-western Hebei,China.Geological Review,49(4):355～360(in Chinese with English abstract).
[34]
Jiang Sihong,Nie Fengjun,Hu Peng and Liu Yan.2006.An important spreading event of the Neo-Tethys ocean during late Jurassic and early Cretaceous:evidence from the zircon U-Pb SHRIMP dating on the diabase in Nagarzê,southern Tibet.Acta Geologica Sinica(English edition),80:522～527.
[35]
Le Maitre R W.1989.A Classification of Igneous Rocks and Glossary of Terms.Oxford:Blackwell,1～193.
[36]
Liang Dingyi,2004.Several important advances in geological surveys on the Qinghai-Tibet Plateau.Geological Bulletin of China,23(1):24～26 (in Chinese with English abstract).
[37]
Mearns,E.W.,1986,Sm-Nd ages for Norwegian garnet peridotite.Lithos,19:269～278.
[38]
Murphy M A,Harrison T M.1999.The relationship between leucogranites and the South Tibetan detachment system,Rongbuk Valley,southern Tibet.Geology,27:831～834.
[39]
Nie Fengjun,Hu Peng,Jiang Sihong,Li Zhenqing,Liu Yan and Zhou Yongzhang,2005.Type and Temporal-Spatial Distribution of Gold and Antimony Deposits (prospects) in Southern Tibet,Tibet Autonomous Region,China.Acta Geologica Sinica(Chinese edition),79(3):373～385 (in Chinese with English abstract).
[40]
Ormerod D S,Hawkesworth C J,Rogers N W,et al.1988.Tectonic and magmatic transitions in the Western Great Basin,USA.Nature,333 (6171-6172):349～353.
[41]
Pan Guitang,Wang Liquan and Zhu Dicheng,2004.Thoughts on some important scientific problems in regional geological survey of the Qinghai-Tibet plateau.Geological Bulletin of China,23 (1):12～19 (in Chinese with English abstract).
[42]
Pearce J A.1983.Role of the sub-continental lithosphere in magma genesis at active continental margins.In:Hawkesworth C J and Norry M J (eds.),Continental basalts and mantle xenoliths.Nantwich:Shiva,230～ 249.
[43]
Ren Jishun and Xiao Liwei,2004.Lifting the mysterious veil of the tectonics of the Qinghai-Tibet plateau by 1:250000 geological mapping.Geological Bulletin of China,23 (1):1～ 11 (in Chinese with English abstract).
[44]
Shao Jian,Li Xianhua,Zhang Lüqiao,Mou Baolei and Liu Baolei.2001.Geochemical condition for genetic mechanism of the Mesozoic bimodal dike swarms in Nankou-Guyaju.Geochimica,30(6):517～527.
[45]
Sun S S and McDonough W F.1989.Chemical and isotopic systematics of oceanic basalts:implications for mantle compositeon and processes.In:Saunders A D and Norry M J (eds.),Magmatism in ocean basins.Geol.Soc.London.Spec.Publ.42,313～345.
[46]
Taylor S R and McClennan S.1985.The continental crust:Composition and evolution.Blackwell Scientific Publications,54:209～230,372.
[47]
Weaver B L.1991.The origin of ocean island basalt end-member compositions:trace element and isotopic constraints.Earth and Planetary Science Letters,104:381～397.
