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本文结合地理、地貌环境和石器工业特点将四川盆地划分为川东平行岭谷区、盆中丘陵区和盆地西缘区,并对三个区域的旧石器时代晚期的石器工业进行比较研究。研究表明川东平行岭谷区、盆中丘陵区的石器工业体现了华南砾石工业的特点,但两者还是有些区别,而盆地西缘区则反映出小石器传统的特点,并有少量细石器文化因素。四川盆地旧石器时代晚期出现的华北小石器工业、细石器文化因素当是由北及南穿越盆地西缘(横断山区东麓)和川东平行岭谷区传播的结果。
Based on the characteristics of geography, geomorphology and stone industry, the paper divides the Sichuan Basin into the parallel Linggou area, the hilly area in the eastern Sichuan basin and the western margin of the basin, and compares the stone industry in the late Paleolithic period in the three regions. The research shows that the stone industry in the area parallel to LingGong and Hilly Basin reflects the characteristics of South China gravel industry, but there are some differences between the two. However, the western margin of the basin reflects the traditional characteristics of small stone tools, Cultural factors. The North China Hearthstone industry and the fine stoneware cultural factors appearing in the Late Palaeolithic period of Sichuan Basin were the result of the transmission from the western margin of the North and South Traversing Basins (east foot of Hengduan Mountains) and the parallel valley region of East Sichuan.