深圳市南山区长岭皮河谷考古调查简报

Brief Report of Field Surveys in the Changlingpi River Valley in Nanshan District of Shenzhen City

长岭皮河为深圳市大沙河支流,河流与两岸丘陵形成一个有较多谷地和低洼地的地理单位,面积约30平方千米。通过对河谷的多次考古田野调查及试掘,先后发现和确认了19处先秦遗址。这些遗址的年代大体可分为三类,即夏末至晚商阶段、西周晚期至春秋时期、主体年代在战国时期下限或可至汉代初期。由各遗址的年代和分布情况可知,此区域在夏商之际至商周之际应为一个大型聚落群。

The Changlingpi River is a tributary of the Dasha River in Shenzhen City.The river,along with the hills on both sides,forms a geographical unit with numerous valleys and low-lying areas,covering an area of approximately 30 square kilometers.Field surveys and test excavations have been conducted in the river valley,confirming the presence of 19 pre-Qin sites.These sites are dated to three periods:the Late Xia to Late Shang period,the Late Western Zhou to Spring and Autumn period,and the Warring States period(possibly also extending to the early Han dynasty).The dates and distribution of these sites suggest a large settlement complex once existed in the surveyed area during the Xia-Shang and Shang-Zhou transitions.