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Chen et al.: Metallogenic setting and material source of Caihong copper-lead-zinc polymetallic deposit 
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APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH 15(3): 651-674. 
http://www.aloki.hu ● ISSN 1589 1623 (Print) ● ISSN 1785 0037 (Online) 
DOI: http://dx.doi.org/10.15666/aeer/1503_651674 
 2017, ALÖKI Kft., Budapest, Hungary 
1167-1196. 
[20] Jiang, C.Y., Wu, W.K., Yang, F., Mo, S.L., and Li, L.C. (1993): Tectonic movement 
during late Caledonian in Tianshan mountain and its geological significance. –Journal of 
Xi’an College of Geology 15: 41-46. (in Chinese with English abstract) 
[21] Jochen, H., Liu, S.F., and Shi, X.F. (2002): Stable isotope geochemistry. –Ocean Press, 
Beijing. 
[22] Klinkhammer, G.P., and Edmond, J.M. (1994): Geochemical implications of rare earth 
element patterns in hydrothermal fluid from mid-ocean ridges. –Geochimica et 
Cosmochimica Acta 58: 5105-5113. 
[23] Liu, Y.S., Hu, Z.C., Gao, S., Günther, D., Xu, J., Gao, C.G., and Chen, H.H.(2008): In 
situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without 
applying an internalstandard. –Chemical Geology 257: 34-43. 
[24] Liu, Y.S., Hu, Z.C., Zong, K.Q., Gao, C.G., Gao, S., Xu, J. and Chen, H.H. (2010): 
Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by 
LA-ICP-MS. –Chinese Science Bulletin 55: 1535-1546. 
[25] Long, L.L., Gao, J., Xiong, X.M., and Qian, Q. (2007): Geochemistry and geochronology 
of granitoids in Bilcai region, southern Central-Tianshan mountains, Xinjiang. –Acta 
Petrologica Sinica 23: 71-73. (in Chinese with English abstract) 
[26] Long, L.L., Wang, J.B., Wang, Y.W., Wang, L.J., Liao, Z., Zhao, L.T., Sun, Z.Y., and 
Gao, L.M. (2015): Sulfur-isotope characteristics and discussion on the source of ore-
forming material of the Xilekuduke Cu-Mo deposit ，Xinjiang Province. –Acta 
Petrologica Sinica 31: 545-554. (in Chinese with English abstract) 
[27] Mills, R., Elderfield, H. (1995): Rare earth element geochemistry of hydrothermal 
deposits from the active TAG Mount, 26°N mid-Atlantic Ridge. –Geochim. Cosmochim. 
Acta 59: 3511-3524. 
[28] Ohmoto, H. (1983): Geologic setting of the Kuroko deposits, Japan: Part I, geologic 
history of the Green Tuff Region. –Econonic Geology 5: 9-23. 
[29] Ohmoto, H. (1996): Formation of volcanic-associated massive sulfide deposits: The 
Kuroko perspective. –Ore Geology Review 10: 135-177. 
[30] Pan, M.H., Jia, Z.L., Ou, J., and Hou, P.B. (2015): Geochemical characteristics of 
sericitolite in Huashigou copper deposit, South Qilian, Gansu. –Geochimica 44: 370-376. 
(in Chinese with English abstract) 
[31] Peng, Y.M., Pan, G.T., and Luo, J.N. (1999): Volcanic-sedimentary characteristics of 
back-arc basin. –Sedimentary Fades and Palaeogeography 19: 65-72. (in Chinese with 
English abstract) 
[32] Piercey, S.J., Peter, J.M., and Mortensen, J.K. (2008): A special issue devoted to 
continental margin massive sulfide deposites and their geodynamic environments. –
Economic Geology 103: 1-10. 
[33] Rees, C.E., Jenkins, W.J., and Monster, J. (1978): The sulfer isotopic composition of 
ocean water sulfate. –Geochimica et Cosmochimica Acta 42: 377-381. 
[34] San, X.L., Xu, S., and Zheng, Y.Z. (2009): Prospecting model of Caihuagou cupriferous 
copperprite deposite in Xinjiang. –XinJiang Geology 27: 32-37. (in Chinese with English 
abstract) 
[35] Sangster, D.F. (1983): Shourt course in sediment-hosted stratiform lead-zinc deposits. –
Mineralogical Association of Canada 8: 6-26. 
[36] Shan, L., Zheng, Y.Y., Xu, R.K., Cao,L., Zhang,Y.L., Lian,Y.L., and Li, Y.H. (2009): 
Review on sulfur isotopic tracing and hydrothermal metallogenesis. –Geology and 
Resource 18: 188-203. (in Chinese with English abstract) 
[37] Shu, L.S., Lu, F.H., Yin, D.H., and Wang, B. (2003): Paleozoic accretion-collision events 
and kinematics of ductile deformation in the Central-Southern Tianshan belt. –Journal of 
Nanjing University(Nature Science) 39: 17-30. (in Chinese with English abstract) 
[38] Simonen, A. (1953): Stratigraphy and sedimentation of the Svecofennidic, early Archean