摘要
绵阳市地处四川盆地西北部,属涪江中游的平坝和浅丘地带,南距成都市约90公里,自西汉设置涪县以来,已有2200多年的建城史,历来为郡、州治所。绵阳境内的崖墓点主要位于涪江中游地区,尤其以涪江与安昌河、芙蓉溪交汇河段的上、
The porcelains unearthed from the cliff burials at Mianyang could be divided into Groups A and B, the dates of which spanned from the Six-Dynasties Period to the early Tang Dynasty. The porcelains of Group A were the products of the local kilns of the Chengdu Plain, the representative one of which was the Qingyang Palace Kiln; that of Group B were the products of the kilns of other regions, which might mainly be the celadon kilns in the middle reach of the Yangtze River. The porcelains of other regions were transported in along with the commercial activities, and then they became the models imitated and reproduced by local kilns, which fundamentally promoted the flourishing of the local porcelain production of Sichuan.
出处
《考古》
CSSCI
北大核心
2017年第1期83-94,共12页
Archaeology
关键词
绵阳崖墓
出土瓷器
分组
分期
窑口
Cliff Burials at Mianyang Unearthed Porcelains Grouping PeriodizationKilns (Production Places)