本文選題：郝家臺(tái)遺址 + 地貌背景　； 參考：《華夏考古》2017年03期

【摘要】：通過(guò)對(duì)郝家臺(tái)遺址探溝剖面和鉆孔資料的分析,并結(jié)合區(qū)域地貌和地層的相關(guān)資料,重建了地貌演化的過(guò)程。郝家臺(tái)遺址的地貌基礎(chǔ)是沖積平原中地勢(shì)相對(duì)較高的天然堤。龍山文化時(shí)期的先民直接在消亡的湖沼之上建立了最初的聚落,并通過(guò)城墻和城壕等設(shè)施的修建以及在城內(nèi)不斷地墊土加高,很好地應(yīng)對(duì)了沖積平原這種不穩(wěn)定的環(huán)境。
[Abstract]:The process of geomorphological evolution was reconstructed by analyzing the data of grooved section and borehole in Hao Jiatai site and combining with the related data of regional geomorphology and strata.The geomorphologic foundation of Hao Jiatai site is the relatively high topographic natural embankment in alluvial plain.The ancestors of Longshan culture built up the initial settlement directly on the dead lake and marsh, and through the construction of city walls and trenches, and the constant increase of soil cushion in the city, the unstable environment of alluvial plain was well dealt with.
【作者單位】： 中國(guó)社會(huì)科學(xué)院考古研究所;北京大學(xué)考古文博學(xué)院;河南省科學(xué)院地理研究所;
【基金】：國(guó)家自然科學(xué)基金項(xiàng)目(41671014) 國(guó)家社科基金重大項(xiàng)目(11&ZD183) 嵩山文化研究會(huì)重大項(xiàng)目的階段性成果
【分類(lèi)號(hào)】：K878
，

本文編號(hào)：1771763