铅同位素组成在古陶产地判别中的应用  

Discrimination of the production sites of ancient pottery by using lead isotopic composition

作　　者：张巽[1] 马林[1] 陈江峰[1] 张兆峰[1] 邱平[2] 王昌燧[2] 

机构地区：[1]中国科学技术大学地球和空间科学系,合肥230026 [2]中国科学技术大学科技史和科技考古系,合肥230026

出　　处：《核技术》2003年第9期693-696,共4页Nuclear Techniques

基　　金：中国科学院重点科研项目"现代考古技术方法基础研究"(KZ-852-J1-418);中国科学院知识创新项目"科技考古的若干前沿研究"(KZCX-N04)资助

摘　　要：对铅同位素组成在鉴别古陶产地上的应用进行了探讨。对采自于河南省贾湖和西山两新石器时代遗址的古陶样品进行了铅同位素组成分析,大部分贾湖样品的铅同位素原子数比^(206)Pb/^(204)Pb为18.0—18.4,^(208)Pb/^(204)Pb为38.4—38.8,而大部分西山样品的铅同位素原子数比^(206)Pb/^(204)Pb为18.6—18.8,^(208)Pb/^(204)Pb为38.7—39.1。因此,对某些产地的古陶,铅同位素组成是鉴别其产地的有力工具。Discrimination of the production sites of ancient pottery by using lead isotopic composition is discussed in this paper. We have determined the lead isotopic compositions of ancient pottery from the Jiahu and Xishan sites, Henan Province. Most of Jiahu pottery show 206Pb/204Pb of 18.0 to 18.4 and 208Pb/204Pb of 38.4 to 38.8, while most of Xishan pottery show 206Pb/204Pb of 18.6 to 18.8 and 208Pb/204Pb of 38.7 to 39.1. Therefore, the lead isotopes are useful in discriminating the production sites of the ancient pottery in some cases.

关 键 词：古陶 铅同位素 贾湖 西山 

分 类 号：K854.2[历史地理—考古学及博物馆学] K876.3[历史地理—历史学]