Evidence of Late Holocene subsidence events in Sporades Islands: Skopelos and Alonnisos

被引：7

作者：

Evelpidou, N. ^{[1
]}

Koutsomichou, I. ^{[1
]}

Pirazzoli, P. A. ^{[2
]}

机构：

[1] Univ Athens, Fac Geol & Geoenvironm, Athens 15784, Greece

[2] Lab Geog Phys, F-92195 Meudon, France

来源：

CONTINENTAL SHELF RESEARCH | 2013年 / 69卷

关键词：

Tidal notches; Palaeoshorelines; Sea level indicators; Aegean; SEA-LEVEL VARIATIONS; NORTH AEGEAN BASIN; TIDAL NOTCHES; SUBMERGED SHORELINES; GREECE;

D O I：

10.1016/j.csr.2013.09.017

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

Through this research relative sea level changes from Late Holocene until the present day were studied, in the area of Skopelos and Alonnisos Islands. The study was accomplished through methodical underwater geomorphological research in both islands and led to the location of six and seven distinct submerged fossil shorelines, in Skopelos and Alonnisos accordingly, along the islands' coastline. Both islands have been affected during the last millennia, by repeated subsidence events, often of coseimic origin. The amount of each subsidence displacement was generally limited to one or a few decimetres, with recurrence intervals of some centuries. (C) 2013 Elsevier Ltd. All rights reserved.

引用

页码：31 / 37

页数：7

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