[1]Zhu Xun, Huang Chongke, Rui Zongyao, et al. Geology of the Dexing Porphyry Copper Orefield[M]. Beijing: Geological Publishing House, 1983.[朱训, 黄崇轲, 芮宗瑶,等. 德兴斑岩铜矿[M]. 北京: 地质出版社, 1983.]
[2]Wang Qiang, Zhao Zhenhua, Jian Ping, et al. SHRIMP dating and Nd-Sr isotopic geochemistry of Dexing granodiorite[J]. Acta Petrologica Sinica,2004, 20(2):315-338.[王强, 赵振华, 简平, 等. 德兴花岗闪长斑岩SHRIMP锆石U-Pb年代学和Nd-Sr同位素地球化学[J]. 岩石学报, 2004, 20(2): 315-338.]
[3]Zhou Q, Jiang Y H, Zhao P, et al. Origin of the Dexing Cu-bearing porphyries, SE China: Elemental and Sr-Nd-Pb-Hf isotopic constraints [J]. International Geology Review, 2012, 54(5): 572-592.
[4]Qiu Junting, Yu Xinqi, Zhang Dehui, et al. LA-ICP-MS zircon U-Pb dating and geological meanings of Tongcun granite porphyry in Kaihua, west Zhejiang province[J]. Geological Bulletin of China, 2011, 30(9): 1 360-1 368.[邱骏挺, 余心起, 张德会, 等. 浙西开化地区桐村花岗斑岩LA-ICP-MS锆石U-Pb年龄及其地质意义[J]. 地质通报, 2011, 30(9): 1 360-1 368.]
[5]Zhu Yudi, Ye Xifang, Zhang Dehui, et al. Petrogeochemistry, SHRIMP dating and Sr-Nd isotopes of Tongcun porphyry Mo-Cu deposit in Kaihua, West Zhejiang province[J]. Geological Review, 2012(in press).[朱玉娣, 叶锡芳, 张德会, 等.浙西开化桐村斑岩型钼铜矿床含矿斑岩岩石地球化学、SHRIMP年代学及Sr-Nd同位素研究[J].地质论评, 2012(待刊).]
[6]Jiang Y H , Zhao P, Zhou Q, et al. Petrogenesis and tectonic implications of Early Cretaceous S-and A-type granites in the northwest of the Gan-Hang rift, SE China[J]. Lithos,2011,121:55-73.
[7]Geological Party of Jinhua, Zhejiang Province. Preliminary Discuss on Relationships between the Characteristics of Porphyries in Kaihua, West Zhejiang Province and Cu-Mo Mineralization[R]. 1982.[浙江金华地质大队专题组. 浙江开化常山一带斑岩体特征与铜钼矿化关系初步探讨[R]. 1982.]
[8]Middlemost E A K. Towards a comprehensive classification of igneous rocks and magmas[J].Earth-Science Reviews,1991, 31(2):73-87.
[9]Frost B R, Barnes C G, Collins W J,et al. A geochemical classification for granitic rocks[J]. Journal of Petrology, 2001, 42(11): 2 033-2 048.
[10]Rui Zongyao, Huang Chongke, Qi Guoming, et al. Porphyry Cu(Mo) Deposites[M]. Beijing: Geological Publishing House, 1984:1-50.[芮宗瑶, 黄崇柯, 齐国明, 等. 中国斑岩铜(钼)矿床[M].北京:地质出版社, 1984:1-50.]
[11]Rui Zongyao, Zhang Lisheng, Chen Zhenyu, et al. Source region discuss on porphyry copper deposits[J]. Acta Petrologica Sinica, 2004, 20(2): 229-238. [芮宗瑶, 张立生, 陈振宇, 等. 斑岩铜矿的原岩或源区探讨[J]. 岩石学报, 2004, 20(2): 229-238.]
[12]Rui Zongyao, Zhang Hongtao, Chen Renyi, et al. Discuss on porphyry copper deposits[J]. Mineral Deposits,2006, 25(4): 491-500.[芮宗瑶, 张洪涛, 陈仁义, 等.斑岩铜矿研究中若干问题探讨[J]. 矿床地质, 2006, 25(4): 491-500.]
[13]Zhu Jinchu, Shen Weizhou, Liu Changshi, et al. Nd-Sr isotopic characteristics and discuss on genesis of Mesozoic granitoids in South China[J]. Acta Petrological et Mineralogical,1990, 9(2): 97-105.[朱金初,沈渭洲,刘昌实,等. 华南中生代同熔系列花岗岩类的Nd-Sr同位素特征及成因讨论[J]. 岩石矿物学杂志,1990, 9(2): 97-105.]
[14]Zhu Jinchu, Jin Zhangdong, Rao Bing, et al. Fluid process of porphyry copper deposits in Tongchang, Dexing district[J]. Journal of Nanjing University (Natural Sciences), 2002, 38(3): 418-434.[朱金初,金章东,饶冰,等. 德兴铜厂铜矿流体过程[J]. 南京大学学报:自然科学, 2002, 38(3): 418-434.]
[15]Wu Liren. Mesozoic granitoids of East China[J]. Acta Petrologica Sinica, 1985, 1(1): 1-10.[吴利仁. 中国东部中生代花岗岩类[J]. 岩石学报, 1985, 1(1): 1-10. ]
[16]Boynton W V. Geochemistry of the rare earth elements: Meteorite studies[C]∥Henserson P ed. Rare Earth Element Geochemistry. Elservier, 1984: 63-114.
[17]Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts: Implications foe mantle composition and processes[J]. Geological Society, 1989, 42:313-345.
[18]Rollinson H R. Using Geochemical Data[M].New York:John hunli Wiley and Sons Inc., 1993.
[19]Chen J F, Jahn B M. Crust evolution of southern China: Nd and Sr isotopic evidence[J]. Tectonophysies,1998, 284: 101-133.
[20]Guo Chunli, Wang Denghong, Chen Yuchuan, et al. Zircon SHRIMP U-Pb dating, elemental and Nd-Sr isotopic geochemistry study of Neoproterozoic granitic complex body of West Sichuan province: Genesis and tectonic implications[J]. Acta Petrologica Sinica, 2007, 23(10): 2 457-2 470.[郭春丽, 王登红, 陈毓川, 等. 川西新元古代花岗质杂岩体的锆石SHRIMP U-Pb年龄、元素和Nd-Sr同位素地球化学研究:岩石成因与构造意义[J]. 岩石学报, 2007, 23(10): 2 457-2 470.]
[21]Gong Rixiang, Lu Chengzhong. Petrogeochemistrical characteristics and tectonic implications of high-K, alkali granitoids in west Zhejiang province[J]. Acta Petrologica Sinica, 2008, 24(10): 2 343-2 351.[龚日祥, 卢成忠. 浙西晚中生代富碱高钾花岗岩类的岩石地球化学特征及构造意义[J]. 岩石学报, 2008, 24(10): 2 343-2 351.]
[22]Shen Weizhou, Lin Hongfei, Wang Dezi, et al. Nd-Sr isotopic study of Mesozoic igneous rock in Zhejiang province[J]. Chinese Journal of Geology, 1999, 34(2): 223-232.[沈渭洲, 凌洪飞, 王德滋, 等. 浙江省中生代火成岩的Nd-Sr同位素研究[J]. 地质科学, 1999, 34(2): 223-232.]
[23]Gao S, Lin W L, Qiu Y M. Contrasting geochemicaland Sm-Nd isotopic compositions of Archaean metasedi-ments from the Kongling high-grade terrain of the Yangtzecraton: Evidence for cratonic evolution and redistribution of REE during crustal anatexis[J]. Geochimica et Cosmochimica Acta, 1999, 63: 2 071-2 088.
[24]Zhang S B, Zheng Y F, Zhao Z F, et al. Neoproterozoic anatexis of Archean litho-sphere: Geochemical evidence from felsic to mafic intrusionsat Xiaofeng in the Yangtze Gorge, South China[J]. Precambrian Research, 2008, 163: 210-238.
[25]Zhang S B, Zheng Y F, Zhao Z F, et al. Origin of TTG-like rocks from anatexis of ancient lower crust: Geochemical evidence from Neoproterozoic granitoids in south China[J].Lithos, 2009, 113:347-368.
[26]Plank T, Langmuir C H. The chemical composition of subducting sediment and its consequences for the crust and mantle[J]. Chemical Geology, 1998, 145: 325-394.
[27]Vervoort J D, Blichert-Toft J, Patchett P J, et al. Relationships between Lu-Hf and Sm-Nd isotopic systems in the global sedimentary system[J]. Earth and Planetary Science Letters, 2000, 168: 79-99.
[28]Barry T L, Saunders A D, Kempton P D, et al. Petrogenesis of Cenozoic basalts from Mongolia: Evidence for the role of asthenospheric versus metasomatized lithospheric mantle sources[J]. Journal of Petrology, 2003,44: 55-91.
[29]Jahn B M, Zhou X H, Li J L. Formation andtectonic evolution of southeastern China and Taiwan:Isotopic and geochemical constraints[J]. Tectonophysics,1990,183:145-160.
[30]Charvet J, Lapierre H, Yu Y. Geodynamicsignificance of the Mesozoic volcanism of southeasternChina[J]. Journal of Southeast Asian Earth Sciences, 1994, 68: 387-396.
[31]Martin H, Bonin B, Capdevila R. The Kuiqiperalkaline granitic complex (SE China): Petrology and geo-chemistry[J]. Journal of Petrology, 1994, 35: 983-1 015.
[32]Lapierre H, Jahn B M, Charvet J. Mesozoic magmatism in Zhejiang province and its relation with the tectonic activities in SE China[J]. Tectonophysics, 1997, 274: 321-338.
[33]Zhou X M, Li W X. Origin of Late Mesozoic igneous rocks in southeastern China: Implications for lithosphere subduction and underplating of mafic magmas[J]. Tectonophysics, 2000, 326: 269-287.
[34]Jiang Y H, Jin G D, Liao S Y, et al. Geochemical and Sr-Nd-Hf isotopic constraints on the ori-gin of Late Triassic granitoids from the Qinling orogen,central China: Implications for a continental arc to continent-continent collision[J]. Lithos, 2010, 117: 183-197.
[35]Condie K C. Plate Tectonics and Crustal Evolution (2nd)[M]: New York: Pergamon Press,1976.
[36]Pearce J A, Harris N B W, Tindle A G. Trace ele-ment discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25: 956-983.
[37]Blevin P L, Chappell B W. The role of magma sources, oxidation states and fractionation in determining the granite metallogeny of eastern Australia[J]. Transactions of the Royal Society of Edinburgh-Earth Sciences, 1992, 83: 305-316.
[38]Blevin P L. Metallogeny of granitic rocks[C]∥The Ishihara Symposium:Granites and Associated Metallogenesis.Geoscience Australia, 2003:1-4.
[39]Ray G E, Webster I C L, Ettlinger A D. The distribution of skarns in British Columbia and the chemistry and ages of their related plutonic rocks[J]. Economic Geology, 1995, 90: 920-937.
[40]Candela. Controls on ore metal ratios in granite-related ore systems—An experimental and computational approach[J].Transactions of the Royal Society of Edinburgh-Earth Sciences,1992, 83: 371-326.
[41]Hedenquist J W, Lowenstern J B. The role of magmas in the formation of hydrothermal ore-deposits[J].Nature,1994, 370:519-527.
[42]Xiao Qinghui,Deng Jinfu, Ma Daquan, et al. Thoughts and Methods of Granitic Study[M]. Beijing: Geological Publishing House, 2002: 71-96.[肖庆辉, 邓晋福, 马大铨, 等. 花岗岩研究思维与方法[M]. 北京: 地质出版社, 2002: 71-96.]
[43]Xu Wengang. The Geochemical Characteristics of the Ore-forming Fluids and Metallogenic Genesis Discussion of the Porphyry Molybdenum (Copper)Deposit of Tongcun in Kaihua, Zhejiang Province[D]. Beijing: China University of Geoscience, 2011. [徐文刚. 浙江开化桐村斑岩钼(铜)矿床成矿流体地球化学及成因讨论[D]. 北京: 中国地质大学, 2011.] |