CAJ | 학술논문

基于黄河下游流域考古遗址中第一次发现的黄泛地层,对苏北梁王城遗址T3902探方南壁剖面上部自然淤积层采样,结合考古断代,并参照历史资料,通过分析重砂矿物和粒度两方面的实验结果,揭示出考古遗址中黄泛地层的沉积物特征.旨在为今后环境考古中对黄泛地层的判别和对比提供可靠的科学依据,特别是为在黄河下游洪泛区考古遗址中疑似黄泛层的确认提供依据.
기우황하하유류역고고유지중제일차발현적황범지층,대소북량왕성유지T3902탐방남벽부면상부자연어적층채양,결합고고단대,병삼조역사자료,통과분석중사광물화립도량방면적실험결과,게시출고고유지중황범지층적침적물특정.지재위금후배경고고중대황범지층적판별화대비제공가고적과학의거,특별시위재황하하유홍범구고고유지중의사황범층적학인제공의거.
On the basis of the Yellow River overflow strata in the archaeological site in the lower Yellow River valley,samples from the natural silt layer on the south wall in unit T3902 in the Liangwangcheng site, heavy mineral and granularity analysis, archaeological dating, and historical data, we studied the properties of the lower Yellow River overflows strata in the Liangwangcheng site. Our study provides a foundation for the interpretation of overflows layers in the borderline of the flood area or provides constraints on the extension of the archaeological site along the lower Yellow River.