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《Journal of Jilin University(Earth Science Edition)》 2006-05
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Studies on the Ar-Ar Age, Pb Isotope Features and Key Factors for the Formation of Fuwan Superlarge Silver Deposit in Guangdong Province

LIANG Hua-ying~ 1 ,YU Heng-xiang~ 2 ,ZENG Ti~ 1 ,XIA Ping~1 1.Key Laboratory for Metallogenic Dynamics, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China 2.Guilin Institute of Technology, Guilin, Guangxi 541004,China  
The Fuwan superlarge silver deposit is hosted in the Early Carboniferous limestones along a contact fault zone between the limestone and the overlying Changkeng Au-hosting siliceous rocks. The ~ 40 Ar-~ 39 Ar age of the ore-related quartz veins from the Fuwan silver deposit is (64.3±0.1) Ma. The silver deposit is characterized by high μ values (10.67~10.95) in Pb isotopic composition, being much higher than those of the Paleozoic ore-hosted strata and being similar to those of ores hosted in Preterozoic metamorphic base in the Western Guangdong Province. It is concluded that the ore-forming material of the superlarge silver deposit came primarily from the Proterozoic basement. The superlarge silver deposit owns its origin to the Himalayan volcanic activities in the region of the Sanshui Basin.The formation of Fuwan superlarge silver deposit is controlled by the following favorable geological conditions: The intersection of deep faults and contemporaneous faults at the margins of the Sanshui Basin served as excellent passageways for ore fluids; the special ore-hosted rock association served as the ore-concentration and ore-trapping structures; the silver-rich basement,multiple stages of mineralization and of mobilization of silver and related elements; geothermal convection system related to multiple episodes of volcanic activities.
【Fund】: 国家自然科学基金项目(49872035 40472049);; 中国科学院创新项目(GIGX-04-03)
【CateGory Index】: P618.52;P597
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