...
首页> 外文期刊>Tectonics >Archaeological record of earthquake ruptures in Tell Ateret, the Dead Sea Fault
【24h】

Archaeological record of earthquake ruptures in Tell Ateret, the Dead Sea Fault

机译:死海断层Tell Ateret地震破裂的考古记录

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

The archaeological Tell Ateret (North Israel), constructed on the active Dead Sea Fault, was intermittently settled for over six millennia. Structures on the Tell that have been offset by earthquake ruptures provide a remarkable record of alternating construction and slip. We excavated the site in order to resolve the geometry and to time the earthquake rupture history back to the earliest settlement. The measurements of faulted archaeological walls are complemented with data from historical documents, numismatic analysis, and geological observations. We report three newly discovered offsets that add to two previously resolved slip events (the 20 May 1202 and 30 October 1759 earthquakes), completing a three millennia archaeoseismic record. The oldest offset measuring at least similar to 2 m bisected Iron Age IIA fortifications. The second offset, the largest of all five, reaching similar to 2.5 m, is dated to circa 142 BCE. The third, whose post-Hellenistic date is not determined, is of similar to 1.5 m, possibly resulting from multiple earthquakes. We constrain the time of the largest offset by a hoard of 45 coins, the latest of which had been minted 143/142 BCE. Indicative pottery and historic texts support the year 143/142 as terminus post-quem of the rupture at this site. These observations, together with a new kinematic approach, show uneven slip distribution in time and variable amounts of slip along the Jordan Gorge segment of the Dead Sea Fault. We suggest, based on previous palaeomagnetic measurements, that distributed deformation west of Tell Ateret can explain the apparent missing slip of 4.5 +/- 3.5 m since the Hellenistic times.
机译:泰勒·阿特雷特(Tell Ateret)考古遗址(北部以色列)建在活跃的死海断裂带上,断断续续地定居了六千年。泰勒(Tell)上已被地震破裂抵消的建筑物提供了交替施工和滑动的显着记录。我们开挖了该地点,以解决几何问题并及时将地震破裂历史追溯到最早的定居点。断层考古墙的测量得到了历史文献,钱币分析和地质观测数据的补充。我们报告了三个新发现的偏移量,这些偏移量增加了两个先前解决的滑动事件(1202年5月20日和1759年10月30日地震),完成了三千年的古地震记录。最早的偏移量至少与2m的铁器时代IIA防御工事相似。第二个偏移量是所有五个偏移量中最大的,达到约2.5 m,可追溯到公元前142年。第三个未确定古希腊时期,大约是1.5 m,可能是由于多次地震造成的。我们用45个硬币ho积来限制最大的偏移时间,最近一次铸造于143/142 BCE。指示性陶器和历史文献支持143/142年,是该地点破裂后的终点。这些观测结果与一种新的运动学方法一起,显示了沿时间的不均匀滑动分布和沿死海断层的约旦峡谷段的滑动量变化。我们建议,根据以前的古地磁测量,Tell Ateret以西的分布变形可以解释自古希腊时代以来出现的4.5 +/- 3.5 m的明显缺失滑移。

著录项

  • 来源
    《Tectonics》 |2015年第10期|2105-2117|共13页
  • 作者单位

    Hebrew Univ Jerusalem, Dept Geog, Jerusalem, Israel;

    Tel Aviv Univ, Dept Geosci, IL-69978 Tel Aviv, Israel;

    Israel Antiqu Author, Dept Coins, Jerusalem, Israel;

    Hebrew Univ Jerusalem, Inst Archaeol, Jerusalem, Israel;

    Hebrew Univ Jerusalem, Inst Archaeol, Jerusalem, Israel;

    Hebrew Univ Jerusalem, Inst Earth Sci, IL-91904 Jerusalem, Israel;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号