爱琴海晚青铜时代的时间表:公元前1700-1400年
Sturt W Manning1, Christopher Bronk Ramsey, Walter Kutschera
1Department of Classics, Cornell University, 120 Goldwin Smith Hall, Ithaca, NY 14853-3201, USA. sm456@cornell.edu
概括
放射性碳年代测定表明,桑托里尼火山爆发发生在公元前17世纪晚期. 对爱琴海晚青铜时代阶段的修订时间表将它们延长了100年,影响了区域历史的相关性.
科学领域:
- 考古学科学 考古学科学
- 通过放射性碳测年法进行测年.
- 青铜时代的时间表
背景情况:
- 确定爱琴海青铜时代的精确时间表对于理解区域相互作用至关重要.
- 传统的约会方法导致了文化阶段的确立时间表,如后米诺伊 IA,IB和II.
- 桑托里尼 (Thera) 喷发是一个重要的古老环境事件,具有潜在的时间标记.
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