河南漯河郝家台遗址的地貌背景初探  

A Preliminary Study of the Geomorphic Background of the Haojiatai Site in Luohe City, Henan Province

作　　者：王辉[1] 张海[2] 鲁鹏[3] 

机构地区：[1]中国社会科学院考古研究所,北京市100710 [2]北京大学考古文博学院,北京市100871 [3]河南省科学院地理研究所,河南郑州市450052

出　　处：《华夏考古》2017年第3期123-130,共8页Huaxia Archaeology

基　　金：国家自然科学基金项目(41671014);国家社科基金重大项目(11&ZD183);嵩山文化研究会重大项目的阶段性成果

摘　　要：通过对郝家台遗址探沟剖面和钻孔资料的分析,并结合区域地貌和地层的相关资料,重建了地貌演化的过程。郝家台遗址的地貌基础是冲积平原中地势相对较高的天然堤。龙山文化时期的先民直接在消亡的湖沼之上建立了最初的聚落,并通过城墙和城壕等设施的修建以及在城内不断地垫土加高,很好地应对了冲积平原这种不稳定的环境。According to the analysis of trench profiles and drilling data at the Haojiatai site, combined with the regional information about landform and stratigraphy, we reconstructed the process of landform changes. The landform foundation of the site was the natural levee relatively high in the floodplain. The ancient people of Longshan culture period built there settlement directly on the disappeared lacustrine bog. They lived on the constantly raised ground in the city and dealt well with the unstable environment of floodplain by the construction of walls and moats.

关 键 词：郝家台遗址 地貌背景 湖沼 天然堤 冲积平原 

分 类 号：K878[历史地理—考古学及博物馆学]