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《Journal of Chengdu University of Technology》 2002-03
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ISOTOPIC COMPOSITION AND GENETIC INDICATION OF SAWAYA′ERDUN GOLD DEPOSIT, XINJIANG

ZHENG Ming hua 1, LIU Jia jun 2, ZHANG Shou ting 3, LONG Xun rong 1 (1.Chengdu University of Technology, China; 2.Institute of Geochemistry, Chinese Academy of Sciences; 3.China University of Geosciences)  
The Sawaya'erdun gold deposit located in the west of Xinjiang is one of the most important gold deposits found in China in the recent years. The deposit occurs in the turbidite sequence of the Middle Upper Carboniferous, and the mimeralization is restricted to the fracture zones developed in the sequence. With layered or lensoid morphology, the orebodies extend in the NE SW trend, being consistent with the extension of the fracture zones. The ore is composed of gold bearing quartz and quartz siderite stringer stockwork with disseminated metal sulfides. Gold in the ore is characterized by microtexture and low fineness and associated with pyrite, arsenopyrite, and chalcopyrite. The lead compositions obtained from the ore are as follows: 206 Pb/ 204 Pb=18.654~18.382; 207 Pb/ 204 Pb=15.470~15.659; 208 Pb/ 204 Pb=38.752~38.062. The δ 34 S values of the metal sulfides analyzed range between 2.61‰ and -1.02‰. The δD values from quartz and siderite vary from -42.5‰ to -72.2‰, the δ 18 O, from 2.94‰ to -11.57‰, and the δ 13 C CO 2 , from -2.35‰ to -10.50‰ . The mineralization dates between 167±18 Ma and 98±9 Ma, using K Ar method. Based on the characteristics of the isotopic composition, it is suggested that the Sawaya'erdund deposit was developed during the late Yanshan movement and the host and underlying strata supplied the source for the mineralization. It could formulate a model of circulating meteoric water becoming a heated hydrothermal at depth, dissolving gold and other metals from the country rocks through which it traversed , and carrying these up to the pressure reduced environment the fracture zones, where they were precipitated because of boiling derived from the reduced pressure. The features of the Sawaya'erdun gold deposit are similar to those of the famous Muruntar gold deposit located in Uzbekistan, and it is the most typical Muruntar type gold deposit discovered so far in China.
【Fund】: 国家“九五”重点科技攻关项目 (96-91 5 -0 4-0 3 ) ;; 国家自然科学基金资助项目 (4 9773 1 97)
【CateGory Index】: P618.51
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