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Relative sea level fluctuations in aegean coastal areas from middle to late holocene

机译:从中全新世到晚全新世爱琴海沿海地区的相对海平面波动

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The current study presents and combines data concerning relative sea level fluctuations from six coastal areas in the Aegean Sea, from Thrace to North-Eastern Crete. These data have been derived from analyses and geo-chronologies on coastal sediments obtained from boreholes in coastal lagoons and from beachrock bends. Trends of relative sea level change at the study areas are presented for the last 6000 years and are compared with K. Lambeck's and A. Purcell [1] estimations for the same areas. It is concluded that sea level is rising faster in Skyros and Mykonos-Delos insular complex of Cyclades islands, mainly due to tectonic movements or lithosphere elastic deformations.
机译:当前的研究提出并结合了有关爱琴海从色雷斯到东北克里特岛的六个沿海地区相对海平面波动的数据。这些数据来自对沿海泻湖钻孔和滩石弯道获得的沿海沉积物的分析和年代学。提出了研究区域近6000年的相对海平面变化趋势,并将其与相同地区的K. Lambeck和A. Purcell [1]估计进行了比较。结论是基克拉迪群岛的Skyros和Mykonos-Delos岛状复合体海平面上升得更快,这主要是由于构造运动或岩石圈弹性变形所致。

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