<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Gaki-Papanastassiou, K.</style></author><author><style face="normal" font="default" size="100%">Evelpidou, N.</style></author><author><style face="normal" font="default" size="100%">Maroukian, H.</style></author><author><style face="normal" font="default" size="100%">Vassilopoulos, A.</style></author></authors><secondary-authors><author><style face="normal" font="default" size="100%">David R. Green</style></author></secondary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Palaeogeographic evolution of the Cyclades Islands (Greece) during the Holocene.</style></title><secondary-title><style face="normal" font="default" size="100%">Coastal and Marine Geospatial Technologies</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><publisher><style face="normal" font="default" size="100%">Springer</style></publisher><pages><style face="normal" font="default" size="100%">297-304</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div&gt;The Cycladic islands are located in the central Aegean Sea (Greece)&amp;nbsp;forming a partly submerged plateau separated into two parts: the eastern shallower&amp;nbsp;one (Andros, Tinos, Mykonos, Naxos, Paros, Syros, Ios, Sikinos, Folegandros)&amp;nbsp;which formed one big island (6.978 km2) at the end of the last glacial period; the&lt;/div&gt;
&lt;div&gt;western islands (Kea, Kythnos, Serifos, Sifnos, Milos) which remained separated&lt;/div&gt;
&lt;div&gt;during the same period. The eastern islands constitute an erosional plateau which&amp;nbsp;is the end product of a Neogene palaeosurface that was partially submerged due to&amp;nbsp;thinning of the crust during the Quaternary. The presence of numerous Neolithic&amp;nbsp;sites both on land and submerged indicates the existence of an advanced civilization&amp;nbsp;in the area for thousands of years. The location of the lost Atlantis could be found&amp;nbsp;in this area probably between Naxos, Paros and Antiparos.&lt;/div&gt;</style></abstract></record></records></xml>