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Significance and Microscopic Analysis of Deformation in the Cultural Remains of Western Zhou Dynasty-Late Spring and Autumn Period at Daijiayuan Ruins in Huoshan,Anhui Province,China

查看全文 作  者:Yao [1]Daquan;Shuo [2]Zhi;Shen [1]Xiaoqi;Chen [1]Anguo;Zheng [1]Yingping;Zheng [1]Haigang;Li [1]Lingli 高影响力作者 机构地区:[1]Earthquake Administration of Anhui Province, Hefei 230031, China;[2]Cultural Relic Archeology Research Institute of Anhui Province, Hefei 230001, China高影响力机构 出  处:《Earthquake Research in China》索引2010年第24卷第3期,共8页高影响力期刊 基  金:This paper is a contribution to Scientific Research Special Project of the Earthquake Calling (200808064);Science and Technology Tackle Key Problem Plan Project of Anhui Province(08010302204);Natural Science Fund of Anhui Province(070415222),China 摘  要:During an excavation survey to the Daijiayuan vestige of the Western Zhou Dynasty-Late Spring and Autumn Period at Huoshan in Western Anhui,a ground crack related to tectonic movement and filled with silty fine sand was found. This phenomenon was initially confirmed to be due to seismic liquefaction. Many microscopic seismic relics,such as load structure,flow structure,cutoff plane and flotation of organic matter were found in the directional microscopic analysis of deformation. These discoveries and cognitions prove that there were two earthquake events taking place in the Western Zhou Dynasty-Late Spring and Autumn Period in this area. Above-mentioned works enrich and develop the research methods to identify prehistoric earthquake event in eastern China area to a certain extent. 关 键 词:中国东部地区 微观分析 西周 晚期 春秋 霍山 变形 安徽省
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