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Discovery of the Natural Deformation Vestige of Gaixia Remains,Guzhen County,Anhui Province,China and Its Implications

Discovery of the Natural Deformation Vestige of Gaixia Remains,Guzhen County,Anhui Province,China and Its Implications
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摘要 Recognition of natural deformation during the excavation of ancient remains and tombs is important for tracing or enriching historic and prehistoric deformation records. Recently, the earthquake agencies,in cooperation with the cultural relics and archaeological institutions, conducted a special excavation investigation to the Gaixia remains archaeological scene in Guzhen,Anhui Province. Faults and fissures were discovered there, which,as demonstrated by the preliminary study,are the traces of two stratum dislocation events of the same period,at a time approximately corresponding to the late Dawenkou culture stage. This work may improve the recognition of earthquake relics in the cultural stratum of humanity in the East China region. Recognition of natural deformation during the excavation of ancient remains and tombs is important for tracing or enriching historic and prehistoric deformation records. Recently, the earthquake agencies, in cooperation with the cultural relics and archaeological institutions, conducted a special excavation investigation to the Gaixia remains archaeological scene in Guzhen,Anhui Province. Faults and fissures were discovered there, which, as demonstrated by the preliminary study, are the traces of two stratum dislocation events of the same period, at a time approximately corresponding to the late Dawenkou culture stage. This work may improve the recognition of earthquake relics in the cultural stratum of humanity in the East China region.
出处 《Earthquake Research in China》 2011年第1期92-100,共9页 中国地震研究(英文版)
基金 sponsored by Scientific Research Special Project of Earthquake Studies(200808064) Science and Technology Tackle Key Problem Plan Project of Anhui Province (08010302204),China
关键词 中国地区 安徽省 遗迹 变形 自然 固镇县 大汶口文化 晚期阶段 Gaixia Archaeological Dawenkou culture Seismic deformation
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