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Lead isotopic study of Shang Dynasty bronzes (13-11 B.C.)and their ore sources

Lead isotopic study of Shang Dynasty bronzes (13-11 B.C.)and their ore sources

作     者:PENG Zi-Cheng ZHANG Zhao-Feng HE Jian-Feng WANG Zhao-Rong(Department of Earth and Space Science, Univcrsity of Sciencc and Technology of China,Hefei 230026)LIU Shi-Zhong(Jiangxi Historical Relic Archaeology Rescarch Institute, Nanchang 330003)HUA Jue-Mi 

作者机构:中国科学技术大学 安徽 合肥 230026 江西省历史考古所 江西 南昌 330003 中科院自然科学史所 北京 100010 

出 版 物:《Nuclear Science and Techniques》 (核技术(英文))

年 卷 期:2000年第11卷第2期

页      面:65-71页

核心收录:

学科分类:0601[历史学-考古学] 06[历史学] 060109[历史学-专门考古] 0807[工学-动力工程及工程热物理] 0827[工学-核科学与技术] 0703[理学-化学] 0702[理学-物理学] 0801[工学-力学(可授工学、理学学位)] 

基  金:中国科学院知识创新工程项目 国家文物局项目 

主  题:商代青铜器  铜矿石材料 同位素比率 考古 商代文明 来源 

摘      要:The Shang Dynasty civilization in China is based on the development of the bronze techniques. A large amount of Shang Dynasty bronzes, excavated from Jiangxi, Hubei and Henan Provinces, have become a focus of world attention. However,the Sha-ng Dynasty center was located at Zhenzhou and Allyang city areas, Henan Province, where no large copper ores have been found so far. Therefore, where did the huge ore material for casting the bronzes come from? It is an unsettled question paid attention by the archaeologists and scicntists. 35 Shang Dynasty bronzes and 21 copper and lead ore materials aged in the Shang-Zhou Dynasty, the Spring-Autumn Period and the modern time, have been measured by the use of mass *** upon lead isotopic ratios, the ore material for casting the bronzes with the middle isotopic ratios of 207Pb/206Pb ranged in 0.8~0.9 could come from the ancient copper mine of Tongling, Jiangxi Province and Tong Lushan, Hubei Province and that with the high isotopic ratios (0.9) could be from the northern part of the Shang Empire, called Gongfang in the historical records, e.g. today’s Hebei and LiaoningProvinces. The others with the low isotopic ratios (0.8) might originate from poly-metalic deposits, with the high isotopic ratios of 238U/204 Pb in the ore flux or in the magma.

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