[1]Dong F X, Li Z J, Chen B L, et al. 1995. The structural control of gold deposits and their exploration in the Dagongshan-Rongdu area of Wuhe county, Anhui Province [M]. Beijing: Geological Publishing House. 1~171 (in Chinese with English abstract).
[14]
[2]Huang D Z, Dai T G, Kong H, et al. 2000. Study on origin of ore-forming fluid of quartz-vein-type deposits in Zhangbaling tectonic zone, Anhui [J]. Geotectonica and Metallogenia,24: 231~236 (in Chinese with English abstract).
[15]
[3]Lanphere M and Dalrymple G B. 1976. Identification of excess 40Ar by the 40Ar/39Ar age spectrum technique [J]. Earth Planet. Sci. Lett., 32: 141~148.
[16]
[4]Li X M, Li B X, Zhang Y, et al. 1985. Isotopic age of Guandian intrusion and dynamic metamorphism of Tanlu fault zone[J]. Journal of University of Science & Technology of China, (Supp.): 254~259 (in Chinese with English abstract).
[17]
[5]Lippolt H J, Fuhrmann U and Hradetzky H. 1986. 40Ar/39Ar age determination of sanidines of the Eifei volcanic field (Federal Republic of Germany): constraints on age duration of a Middle Pleistocence cold period [J]. Chem. Geol. (Isot. Geosci. Sect.), 59: 187~204.
[18]
[6]Liu J M, Chen B L, Meng X G, et al. 1998. Geological and geochemical properties of Dagongshan gold deposit, Wuhe, Anhui, and its genesis [J]. Mineral Deposits, 17(Supp.): 303~306 (in Chinese).
[19]
[7]Qiu H N, Dai T M and Pu Z P. 1995. The implication of spectra of trace K minerals from the Lushui tengsten-tin deposit, Yunnan Province[J]. Mineral Deposits, 14(3): 273~280 (in Chinese with English abstract).
[20]
[8]Qiu R L. 1998. Geology and geochemistry of gold deposits in Zhangbaling region [J]. Mineral Deposits, 17(Supp.): 335~338 (in Chinese).
[21]
[9]Sang H Q, Wang S S, Hu S L, et al. 1994. 40Ar/39Ar dating method and Ar isotope mass spectrometry analysis of quartz [J]. Journal of Chinese Mass Spectrometry Society, 15(2): 17~27 (in Chinese with English abstract).
[22]
[10]Tang Y C, Wu Y C, Chu G Z, et al. 1998. Geology of copper-gold polymetallic deposits in the along-Changjiang area of Anhui Province [M]. Beijing: Geological Publishing House. 1~351 (in Chinese with English abstract).
[23]
[11]Wan T F, Zhu H, Zhao L, et al. 1996. Formation and evolution of Tancheng-Lujiang fault zone: A review[J]. Geosciences, 10(2): 159~167 (in Chinese with English abstract).
[24]
[12]Wang S S, Sang H Q, Hu S L, et al. 1985. Application of the 49-2 reactor to 40Ar/39Ar dating and the geological significance of age spectra of amphibolite from Caozhuang Group, Qian\'an[J]. Acta Petrologica Sinica, 2(2): 36~42 (in Chinese with English abstract).
[25]
[13]Wang X F, Li Z J, Chen B L, et al. 2000. Tan-Lu fault belt [M]. Beijing: Geological Publishing House, 1~374 (in Chinese with English abstract).
[26]
[14]Yang J H and Zhou X H. 2000. The Rb-Sr isochron of ore and pyrite sub-samples from Linglong gold deposit, Jiaodong Peninsula, eastern China, and their geological significance[J]. Chinese Science Bulletin, 45(24): 2272~2277.
[27]
[15]Zeitler P K and Gerald J D F. 1986. Saddle-shaped 40Ar/39Ar age spectra from young, microstructurally complex potassium feldspars [J]. Geochim. Cosmochim. Acta, 50: 1185~2119.