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作 者:彭子成[1] 梁宝鎏[2] 余均岳[2] 李果[3] 李德卉[2] 周静[1]
机构地区:[1]中国科学技术大学地球和空间科学学院,安徽合肥230026 [2]香港城市大学物理及材料科学系 [3]香港城市大学中国文化中心
出 处:《文物保护与考古科学》2007年第1期1-7,共7页Sciences of Conservation and Archaeology
基 金:香港城市大学CERG(SRG-Fd-7001721;7010087)项目;国家自然科学基金(40676069)
摘 要:用探针型能量色散X荧光光谱技术测定元-明年代的香港青釉瓷、元-明年代的广东青釉瓷、宋-元年代的福建青釉瓷样品的化学组成,用胎式、釉式和主成分分区的方法,研究了香港样品主要来源于广东青瓷窑场的制品,部分来源于福建青釉瓷产品。它们同属于南方青釉瓷系列,但是其胎质成分与浙江龙泉的正宗青釉瓷不同。然而,釉式的组成分布显示,香港、广东青瓷釉与龙泉青瓷釉的化学成分有部分的重叠,表明前两处的仿龙泉青瓷釉在外观上与正宗的产品有相似的质素。The celadon excavated from the Yuan - Ming Dynasty stratigraphy of Hong Kong,together with that from the Yuan- Ming Dynasty stratigraphy of Guangdong and that from the Song- Yuan Dynasty stratigraphy of Fujian have been investigated by using the micro- EDXRF technique. The body modes and principal component analysis of the celadon showed that most part of the Hong Kong celadon was from the products made in Guangdong kilns,and some part of the Hong Kong celadon were from the made in Fujian kilns.'Iherefore, the Hong Kong celadon belongs to the southem celadon system while the glaze mode of the Hong Kong celadon was different from that of Longquan celadon.3he results also showed that the chemical composition of the three places were partly similar.It means that the imitative celadon excavated from Hong Kong and Guangdong areas have a fine appearance,which was similar to the true products made in the Longqtmn kilns,Zhejiang.
关 键 词:微探针型X荧光光谱技术 香港青釉瓷残片 化学组成 源区判别
分 类 号:K876.3[历史地理—考古学及博物馆学] O571.33[历史地理—历史学]
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