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《Journal of Jilin University(Earth Science Edition)》 2007-04
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Sedimentary Exhalative Origin of the Baiyinnuoer Zinc-Lead Deposit,Chifeng,Inner Mongolia:Geological and Sulfur Isotope Evidence

ZENG Qing-dong1,LIU Jian-ming1,JIA Chang-shun2,WAN Zhi-min3,YU Chang-ming1,YE Jie1,LIU Hong-tao11.Key Laboratory of Mineral Resources Institute of Geology & Geophysics/ Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China2.School of Civil and Environmental Engineering,Beijing University of Science and Technology,Beijing 100083,China3.Baiyinnuoer Zinc-Lead Mine,Chifeng,Inner Mongolia 025473,China  
Baiyinnuoer zinc-lead deposit in Chifeng,Inner Mongolia,is located at the middle segment of the Da Hinggan Mountains,in the Permian Huanggangliang Group.The distribution of the ore bodies are controlled by fold structures.The ore bodies are mainly composed of layered,disseminated and massive ores.The mineralization can be divided into two periods: the early mineralization including layered,layer parallel veined and brecciated ores,and the late mineralization including veinlets and veined ores.The sulfur isotopic compositions of the sulfides from ores show that the values(average-4.31‰) of the δ34S of the early mineraliztion ores are clearly lower than that(average-1.83‰) of the late mineralization ores.Comprehensive studies indicate that the Baiyinnuoer zinc-lead deposit is a type of sedimentary exhalative Zn-Pb-Ag deposit and superimposed by Yanshanian magma hydrothermal activity.The main metallogenic period is the Permian.
【Fund】: 国家“973”项目(2006CB403500);; 赤峰市白音诺尔铅锌矿资助
【CateGory Index】: P618.4
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