［1］Chen F W, Li H Q, Cai H, et al. 1999. The origin of the Jinwozi gold deposit in eastern Xinjiang-evidence from isotope geochronology[J]. Geol. Rev., 45(3): 247～254 (in Chinese with English abstract).
[4]
［2］Chen Z Y, Zhang X Q, Zhang Z M, et al. 1993. The geological deve-lopment and regional metallogenic model for gold of the Beishan area [J]. Uranium Geol., 9(2): 65～75 (in Chinese with English abstract).
[5]
［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: 7～27.
[6]
［6］Huang C K, Bai Y, Zhu Y S, et al. 2001. Copper deposit of China [M]. Beijing: Geol. Pub. House. 153～157(in Chinese).
[7]
［7］Li H Q, Xie C F and Chang H L. 1998. Metallogenic geochronology of nonferrous and precious metal deposits of northern Xinjiang[M]. Beijing: Geol. Pub. House. 1～256 (in Chinese with English abstract).
[8]
［8］Liu X Y and Wang Q. 1995. Tectonics of the orogenic belts in Beishan Mt. Western China and their evolution[J]. Geol. Research (Dixueyanjiu), 28: 37～48 (in Chinese with English abstract).
[9]
［9］Mao J W, Yang J M, Qu W J, et al. 2002. Re-Os dating of Cu-Ni sulfide ores from Huangshandong deposit in Xinjiang and its geodynamic significance[J]. Mineral Deposits, 21(4): 323～330(in Chinese with English abstract).
[10]
［10］Nie F J, Jiang S H, Zhao X M, et al. 2000. Type and evolution of the gold deposits in the Beishan region [J]. J. Changchun University of Science and Technology, 31(Special Issue on Gold Deposits): 21～26 (in Chinese with English abstract).
[11]
［11］Nie F J, Jiang S H, Bai D M, et al. 2002a. Temporal-spatial distribution and metallogenic dynamic processes of gold deposits occurring in the southern part of the Beishan, northwestern China[A]. In: Chen Y C, ed. Academic papers of 80th anniversary of the Geological Society of China[C]. Beijing: Geol. Pub. House. 293～299(in Chinese).
[12]
［12］Nie F J, Jiang S H, Bai D M, et al. 2002b. Metallogeny and ore-prospecting of ore deposits occurring within the conjunction area of Inner Mongolia, Gansu and Xinjiang (Beishan Mt.), northwest China[M]. Beijing: Geol. Pub. House. 1～499(in Chinese with English abstract).
[13]
［13］Nie F J, Jiang S H, Bai D M, et al. 2003. Type and temporal-spatial distribution of metal deposits in the Beishan mountains, Inner Mongolia, and its neighboring region [J]. Acta Geologica Sinica, 77(3):367～377(in Chinese with English abstract).
[14]
［18］Xi X P. 1997. Geology and gold prospecting target of the Jinwozi rock body [J]. Xinjiang Geol., 15(1): 76～83 (in Chinese with English abstract).
[15]
［19］Zeng C H, Chen J M and Li X C. 1997. Controlling factors and ore genesis of the Mazhuangshan gold deposits, Xinjiang [J]. Gold Geol., 3(4): 55～63(in Chinese with English abstract)
[16]
［20］Zhou J Y, Zhang B, Zhang C W, et al. 1996. Geology of silver, rhe-nium-molybdenum, gold and copper deposits occurring within the eastern Tianshan ancient continent and along its margin [M]. Beijing: Geol. Pub. House. 1～191 (in Chinese with English abstract).
［3］Cui H W and Chen Z Y. 1996. Geology of gold deposits in Beishan region [M]. Beijing: Geol. Pub. House. 1～104 (in Chinese with English abstract).
[29]
［4］Gansu Bureau of Geology and Mineral Resources (GBGMR). 1989. Regional geology of Gansu Province[M]. Beijing: Geol. Pub. House. 1～692 (in Chinese with English abstract).
[30]
［14］Qin K Z, Sun S, Li J L, et al. 2002. Paleozoic epithermal Au and porphyry Cu deposits in North Xinjiang, China: epochs, features, tectonic linkage and exploration significance[J]. Resource Geology, 52(4): 291～300.
[31]
［15］Robert F. 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: 7～17.
[32]
［16］Wang D W, Zou Z P and Li S X. 1995. On the ore-forming geological features and ore deposit genesis of the Gongpoquan copper deposit, Gansu Province [J]. Northwest Geoscience, 16(1): 115～122 (in Chinese with English abstract).
[33]
［17］Wang F Q. 1996. Rb-Sr isochron ages and the characteristics of REE distribution patterns of two stages of intrusive bodies correlated with Baishantang copper ore deposits [J]. Bulletin of Mineralogy, Petrology and Geochemistry, 15(3): 187～190 (in Chinese with English abstract).
