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西安半坡仰韶文化遗址的地学解析
引用本文:戴宏1,丁华2,3,屈茂稳2,刘文红2. 西安半坡仰韶文化遗址的地学解析[J]. 延边大学学报(自然科学版), 2007, 0(3): 269-273
作者姓名:戴宏1  丁华2  3  屈茂稳2  刘文红2
作者单位:1.长安大学校长办公室,陕西西安710064;2.长安大学地球科学与资源学院,陕西西安710054;3.西北大学城市与资源学系,陕西西安710069;
摘    要:以地学背景分析为基础,探讨了地学背景与半坡仰韶文化遗址的关系。半坡仰韶文化遗址位于新构造运动形成的渭河地堑内的西安凹陷,地学背景对于半坡仰韶文化遗址的形成具有重要意义,重点体现在新构造运动奠定了文化遗址形成的环境背景,区域水系及地貌结构为半坡先民提供了良好生活环境,秦岭北坡及附近的岩石为石质工具的物质来源等方面。

关 键 词:仰韶文化  半坡遗址  地学背景  西安凹陷

Geological Analysis of Banpo Yangshao Culture Relic in Xi'an City
DAI Hong1,DING Hua2,' target="_blank" rel="external">3,QU Mao-wen2,LIU Wen-hong2. Geological Analysis of Banpo Yangshao Culture Relic in Xi'an City[J]. Journal of Yanbian University (Natural Science), 2007, 0(3): 269-273
Authors:DAI Hong1,DING Hua2,' target="  _blank"   rel="  external"  >3,QU Mao-wen2,LIU Wen-hong2
Affiliation:1. President O ffice, Chang'an University, Xi'an 710054, Shaanxi, China; 2. School of EarthSciences and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 3. Departmento fUrban and Resources, Northwest University, Xi'an 710069, Shaanxi, China
Abstract:This paper analyzes the geological background and the relationship between the background and BanpoYangshao culture relic. Banpo relic is located in Xi'an depression of Weihe graben formed by the neotectonicmovement, the geological background is important for the formation of Banpo relic. Neotectonic movement lays afoundation for the environment, geomorphic feature supplies Banpo people with a good environment, rocks ofnorth slope of Qinling Mountain are the sources of stone tool.
Keywords:Yangshao culture  Banpo relic  geological background  Xi'an depression
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