徐夕生,邓平,O\'Reilly S Y,Griffin W L,周新民,谭正中.2003.华南贵东杂岩体单颗粒锆石激光探针ICPMS U-Pb定年及其成岩意义.科学通报,48(12):1328~1334.
[7]
章崇真.1975.某钽铌铍矿花岗岩岩石化学特征.地球化学,(2):249~257.
[8]
Carter A, Roques D, Bristow C, Kinny P. 2001. Underestanding Mesozoic accretion in Southeast Asia: Significance of Triassic thermotectonism (Indosinian orogeny) in Vietnam. Geology, 29:211~214.
[9]
Ching-Ying Lan, Sun-Lin Chung, Jason Jiun-San Shen, Ching-Hua Lo, Pei-ling Wang, Tran Trong Hoa, Hoang Huu Thanh,Stanley A Mertzman. 2000. Geochemical and Sr-Nd istopic Characteristics of granitic rocks from northern Vietnam. Journal of Asian Sciences, 18: 267~280.
[10]
Lu Huanzhang,Shi Jixi, Yu Cimei. 1974. Study of the temperature of diagenesis and mineralization in the Huanan X deposit area.Geochemica, (3): 145~153 (In Chinese).
[11]
Sun Gong\'an, Shi Mingkui, Zhang Hongliang, Hu Xiongwei. 1985.The petrology, geochemistry and metallization of the Dajishan granit. Research Reports of the Geology and Mineral Resouces of Nanling. Wuhan: China University of Geosciences P R. 326~363(In Chinese).
[12]
Xu Xisheng, Deng Ping, O\'Reilly S Y, Griffin W L, Zhou Xinming,Tan Zhengzhong. 2003. Single zircon LAM-ICPMS U-Pb dating of the Guidong complex (SE China) and its petrogenetic significance. Chinese Science Bulletion, 48 (12) : 1328 ~ 1334 (In Chinese).
[13]
Yuan Zhengxin, Chen Sheng, Huang Fuqiang, Song Guoyun, Wu Yuning. 1985. Characteristics of tectonic evolution and its relation to rock-forming and mineralization in the Nanling Area in the Mesozoic and Cenozoic times. Research Reports of the Geology and Mineral Resouces of Nanling. Wuhan: China University of Geosciences P R. 54~79.
[14]
Zhuang Longchi, Lin Weisheng, Xie Tinghuan. 1991. Stable isotope geochemistry of Dajishan tungsten mine in Jiangxi Province. Bull.Yichang Inst. Geol. Mineral Resources, CAGS, (16): 109~120(In Chinese).
Chen Peirong, Hua Renmin, Zhang Bangtong, Lu Jianjun, Fan Chunfang. 2002. Early Yanshanian post-orogenic granitoids in the Nanling region. Science in China (Series D) 45 (8): 4~15 (In Chinese).
[24]
Claude L, Henri M, Nguyen V V, Delphing R, Valerica A, Claude R. 1997. Indosinian NW-trending shear zones within the Truong Son belt (Vietnam) 40 Ar-39 Ar Triassic ages and Cretaceous to Cenozoic overprints. Tectonophysics, 283: 105~127.
[25]
Hua Renmin, Chen Peirong, Zhang Wenlan, et al. 2003,Metallogenic systems related with Mesozoic and Cenozoic granitoids in South China. Science in China(Series D), 33 (4):335~343 (In Chinese).
[26]
Krogh T E. 1973. A low contamination method for hydrothermal decomposition of zircon and extraction of U and Pb for isotopic age determinations. Geochim et Cosmochim Acta, 37:485~494.
[27]
Pupin J P. 1980. Zircon and granite petrology. Contrib. Mineral.Petrol. , 73: 207~220.
[28]
Wang Yuejun, Zhang Y, Fan Weiming, Xi Xianwu, Guo Feng, Lin Ge. 2002. Numerical modelling of the formation of Indo-Sinian peraluminous granitoids in Hunan Provinces: Basaltic underplating versun tectonic thickening. Science in China (series D), 45 (11) :1042~1056.
[29]
Zhang Chongzhen. 1974. A case granit of Ta-Nb-W-Be mineralization. Geochemica, (4): 249~257 (In Chinese).
[30]
Zhang Chongzhen. 1975. Petrochemistical characteristics of granitoid of a Ta-Nb-W-Be mineralization. Geochemica. (2): 135~145(In Chinese).