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Archaeological and geophysical investigation of submerged coastal structures in Kekova, southern coast of Turkey

机译:土耳其南部海岸Kekova淹没沿海结构的考古和地球物理调查

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摘要

We conducted archaeological and geophysical surveys in order to investigate the submergence of ancient constructions along the coast at Kekova Island in southern Turkey. Submerged archaeological remains were measured with respect to present sea level, and geological features that may have caused subsidence were determined by seismic investigation. We estimated relative sea-level change taking into account presumed original elevation of constructions associated with the harbor at the time of occupation and compared our results with eustatic-isostatic sea-level studies in the Mediterranean. Ceramics found along the submerged quay of Kekova Island provided evidence for the time of last use of the harbor structures and suggest that submergence began during the early Byzantine period. Considering relative sea-level changes, eustatic-isostatic effects, and the period of submergence, we estimate a rate of coastal tectonic subsidence of at least 1.6 mm/yr over the last 1400 years.
机译:我们进行了考古和地球物理调查,以调查土耳其南部Kekova岛沿岸古代建筑的淹没情况。根据当前海平面测量淹没的考古遗迹,并通过地震调查确定可能引起沉陷的地质特征。我们估计了相对海平面的变化,同时考虑了占领时与海港有关的建筑物的原始标高,并将我们的结果与地中海地区的等静压海平面研究进行了比较。在科科娃岛(Kekova Island)淹没码头附近发现的陶瓷为最后一次使用海港结构提供了证据,并表明淹没始于拜占庭早期。考虑到相对的海平面变化,等静线效应和淹没期,我们估计过去1400年中海岸构造沉降的速率至少为1.6 mm / yr。

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