略论三台后底山崖墓的年代及相关问题

Discussions on the Houdishan Cliff-tomb in Santai County,Sichuan

根据对出土随葬品的类型学分析,后底山崖墓可划分为A、B两组,A组可以视作是一次下葬,年代约在南朝中晚期,晚到隋代的可能性较小;B组可能属于两次或多次下葬,年代应在南朝中晚期至唐代早期之间。三台境内汉唐时期崖墓的地域分布范围呈现出随时代而变化的特点,即由南部的郪江流域向中、北部的涪江流域移动,而导致这一变化趋势的主要因素在于该地区的历史沿革及县治的迁移变动。

According to the typological studies of burial artifacts which have been unearthed,it is appropriate to divide Houdishan cliff-tomb into group A and group B.We can infer that group A was interred once and it was much more likely built in the middle-late of the Southern Dynasty.It seems that group B was interred at least twice and its age may between middle-late of the Southern Dynasty and early in the Tang Dynasty.In Santai county,it can be recognized that the geographical distribution of cliff-tombs from Han Dynasty to Tang Dynasty changed with age,which means they ranged from the south part to the central and the north part.In another words,from the Qijiang river basin to the Fujiang river basin.The historic evolution of this region and the migrations of the county seat are the main factors that attributed to this variation trend.