[1]Chen B W, Wang Y B and Zuo G C. 1995. Terrain subdivision of the northern Qinghai-Xizang9Tibet)plateau and its tectonic evolution[J]. Acta Geophysica Sinica, 38(Supp.Ⅱ): 98~113 (in Chinese with English abstract).
[2]
[2]Chil-Sup S and Seong-Taek Y. 1997. Jurassic mesothermal gold mineralization of the Samhwanghak mine, Youngdong area, Republic of Korea:Constraints on hydrothermal fluid geochemistry[J]. Econ. Geol., 92: 60~80.
[3]
[4]Goldfarb R J, Phillips G N and Nokleberg W J. 1998. Tectonic setting of synorogenic gold deposits of the Pacific Rim[J]. Ore Geol. Rev., 13(1~5): 185~218.
[4]
[5]Groves D I, Goldfarb R J, Gebre-Mariam M, et al. 1998. Orogenic gold deposits: A proposed classification in the context of their crustal distribution and relationship to other gold deposit types[J]. Ore Geol. Rev., 13 (1-5): 7~27.
[5]
[6]Groves D I, Goldfarb R J, Knox-Robinson C M, et al. 2000. Lake-kinematic of orogenic gold deposits and significance for computer-based exploration techniques with emphasis on the Yilgarn Block, Western Australia[J]. Ore Geol. Rev., 17(1-2): 1~38.
[6]
[7]Jiang C F, Yang J S, Feng B G, et al. 1992. Opening closing tectonics of Kunlun mountains[A]. In:Geological Memoirs, 5(12)[C]. Beijing:Geological Publishing House. 1~224 (in Chinese).
[7]
[8]Jiang N, Xu J H and Song M X. 1999. Fluid inclusion characteristics of mesothermal gold deposits in the Xiaoqinling district, Shaanxi and Henan Provinces, People\'s Republic of China[J]. Mineralim Deposita, 34: 150~162.
[8]
[9]Kerrich R and Wyman D A. 1990. The geodynamic setting of mesothermal gold deposits: An association with accretionary tectonic regimes[J]. Geology, 18: 882~885.
[9]
[10]Kerrich R. 1993. Perspectives on genetic models for lode-gold deposits[J]. Mineralium Deposita, 28: 362~365.
[10]
[11]Kerrich R and Cassidy K F. 1994. Temporal relationships of lode-gold mineralization to accretion, magmatism, metamorphism and deformation, Archean to present: A review[J]. Ore Geol. Rev., 9: 263~310
[11]
[12]Kerrich R, Goldfarb R, Groves D, et al. 2001. The characteristics, origins and geodynamic settings of supergiant gold metallogenic provinces[J]. Science in China(series D), 43(supp.): 1~68.
[12]
[13]Lindgren W. 1933. Mineral Deposits[M]. 4th ed. New York and London: McGraw Hill. 930.
[13]
[14]Martin H. 1987. Petrogenesis of Archaean trondhjemites, tonalites, and granodiorites from eastern Finland: major and trace element geochemistry[J]. Journal of Petrology, 28: 921~953.
[14]
[15]Martin H. 1993. The mechanisms of petrogenesis of the Archaean continental crust-comparison with modern processes[J]. Lithos, 30: 373~388.
[15]
[16]Poulsen K H. 1996. Lode-gold. In: Eckstrand O R, Sinclair W D, Thorpe R I ed. Geology of Canadian Mineral Deposite Types. The Geology of North America[C]. Geol. Soc. Am., P-1: 323~328.
[16]
[17]Witt W K and Vanderhor F. 1998. Diversity within a unified model for Archean gold mineralization in the Yilgarn Craton of Western Australia: An overview of the late-orogenic, structually-controlled gold deposits[J]. Ore Geol. Rev., 13 (1~5): 29~64.
[17]
[18]Yin H F and Zhang K X. 1998. Evolution and characteristics of the central orogenic belt[J]. Earth Science-Journal of China University of Geosciences, 23(5): 437~442 (in Chinese with English abstract).
[18]
[19]Zhang D Q, Feng C Y, Li D X, et al. 2001. Orogenic gold deposits in the North Qaidam and East Kunlun Orogen, West China[J]. Mineral Deposits, 20(2): 137~146 (in Chinese with English abstract).
[19]
[20]Zhang S H. 2000. Study on ore-controlling structures, tectonic stress field and ore-forming mechanism in Saibagou area, Wulan County, Qinghai Province[D]. Beijing: Institute of Geomechanics, CAGS, 1~71 (in Chinese with English abstract).
[20]
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[21]
[21]Zhou X Q, Song Y G, Deng J, et al. 1996. A study of structural control of ores in the Dulan area, Qinghai[J]. Journal of Geomechanics, 2(1): 34~41 (in Chinese with English abstract).
[3]Fu Q Y and Li B L. 1998. Metallogenetic features and ore-controlling conditions of the Saibagou gold deposit, Qinghai[J]. Geol. of Qinghai, 7(1): 43~49 (in Chinese with English abstract).