地震地质 ›› 2010, Vol. 32 ›› Issue (2): 244-251.DOI: 10.3969/j.issn.0253-4967.2010.02.007

• 研究论文 • 上一篇    下一篇

安徽固镇垓下遗址自然变形遗迹的发现及特征初探

姚大全1, 朔知2, 刘加灿1, 唐杰平3, 王志2, 沈小七1, 陈安国1, 郑海刚1   

  1. 1. 安徽省地震局, 合肥, 230031;
    2. 安徽省文物考古研究所, 合肥, 230001;
    3. 安徽省铜陵市文物管理局, 铜陵, 244001
  • 收稿日期:2009-07-09 修回日期:2009-08-29 出版日期:2010-06-29 发布日期:2010-09-01
  • 作者简介:姚大全,男,1956年生,1987年毕业于合肥工业大学构造地质专业,获理学硕士学位,研究员,多年来一直从事地震地质、活动构造和史前地震事件的识别研究工作,电话:0551-5571484,E-mial:daquany@aheq.gov.cn.
  • 基金资助:
    中国地震局地震行业科研专项(200808064);安徽省科技攻关计划项目(08010302204)共同资助

DISCOVERY OF NATURAL DEFORMATION VESTIGE AT GAIXIA RUINS,GUZHEN COUNTY,ANHUI PROVINCE AND ITS IMPLICATIONS

YAO Da-quan1, SHUO Zhi2, LIU Jia-can1, TANG Jie-ping3, WANG Zhi2, SHEN Xiao-qi1, CHEN An-guo1, ZHENG Hai-gang1   

  1. 1. Earthquake Administration of Anhui Province, Hefei 230031, China;
    2. Cultural Relic Archeology Research Institute of Anhui Provine, Hefei 230001, China;
    3. Institute of Cultural Relic Archeology of Tongling City, Anhui Province, Tongling 244001, China
  • Received:2009-07-09 Revised:2009-08-29 Online:2010-06-29 Published:2010-09-01

摘要: 古遗址、墓地发掘过程中自然变形的识别研究是反演或充实历史或史前地震变形资料的重要工作。地震部门与文物考古部门合作,对安徽固镇垓下遗址考古现场进行了专题发掘研究,发现了断层和裂缝,初步研究显示为同期2次层位变动事件的遗迹,发生时代约相当于大汶口文化晚期,该工作有助于推动中国东部人类文化层中地震遗迹的识别。

关键词: 考古, 大汶口文化, 地震变形, 垓下

Abstract: Recognition of natural deformation during excavating ancient ruins and tomb is an important work of tracing or enriching the history and the historic records about prehistoric deformation.Recently,the earthquake department in cooperation with the cultural relic archaeology department conducted the special excavation research at the archaeological site of Gaixia ruins,Guzhen,Anhui,and discovered fault and cracks,which are demonstrated by preliminary study to be the vestiges of two coeval strata deformation events.The high speed deformation characteristic possibly represents two strong earthquake events,and the time is approximately in the Late Dawenkou culture stage.The crack was formed earlier than the fault.The discovery is the first in the eastern China.This work has filled the gap of research on recognition of natural dislocation event in Late Dawenkou culture stage and may improve the recognition of seismological relics in cultural stratum of human being in eastern China,especially in the transition belt between the north and south of China in the Changjiang-Huaihe area.

Key words: archaeology, Dawenkou culture, seismic deformation, Gaixia

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