西西里岛东北部奥兰多角可能发生公元6 -7世纪地震的考古证据调查

C. Bottari, A. Bottari, P. Carveni, M. Mastelloni, M. Olla, U. Spigo
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引用次数: 1

摘要

Capo d 'Orlando考古遗址位于西西里岛东北部,在罗马和拜占庭时期(公元3世纪至7世纪),人们密集居住,在此期间,一座浴场建筑群可能与一座延伸到海边的大型别墅有关。考古地震研究表明,在拜占庭时期(公元6 -7世纪),这个建筑群遭受了破坏:(1)浴池倒塌,(2)平行的干砖墙向同一方向倾斜,(3)浴池地板开裂。这种破坏可能是由地震事件造成的,破坏程度表明强烈的震动。关于公元1000年之前地震的历史记录可能并不完整。实际上,在这段时间内,只有四次地震在地震文献中被模糊地报道过。缺乏地震事件的历史报告并不一定意味着发生过地震。考古地震资料表明,该岛并不是静止的,相反,它遭受了几次地震。本文的分析基于详细的现场调查,主要处理地震原因,但也考虑到与观测到的破坏有关的其他可能原因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Investigation of Archaeological Evidence for a Possible 6th-7th Century AD Earthquake in Capo d'Orlando (NE Sicily)
The archaeological site of Capo d’Orlando, located in NE Sicily was intensively inhabited during the Roman and Byzantine periods (3rd to the 7th century AD) during which a bath complex probably associated to a large villa extending seawards was built. Archaeoseismological research shows that during the Byzantine period (6th -7th century AD) this complex suffered damage: (1) collapse of the bath, (2) tilting of parallel dry masonry walls in the same direction, and (3) cracking of the floor in the bath. This damage might have been produced by a seismic event, where the level of destruction indicates a strong shaking. The historic record of earthquakes prior to the year 1000 AD is probably not complete. Actually, only four earthquakes are vaguely reported in the seismic literature for this time span. This lack of historical reports on seismic events does not necessarily mean that any earthquakes happened. Archaeoseismic data show that the island was not quiescent but on the contrary suffered several earthquakes. The analysis presented here, based on detailed site surveys, deals principally with seismic causes but it also takes into account other possible causes with regard to the observed damage.
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