<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>47</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Papadopoulou-Vrynioti, K</style></author><author><style face="normal" font="default" size="100%">Vassilopoulos, A.</style></author><author><style face="normal" font="default" size="100%">Evelpidou, N.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Correlation of the configuration of the slopes of Yliki and Paralimni (Viotia) with the tectonics.</style></title><secondary-title><style face="normal" font="default" size="100%">Water in 21st century: Problems-Prospects Conference</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2003</style></year></dates><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;In this paper the area of Iliki and Paralimni karstic lakes is studied through&lt;br&gt;fieldwork and GIS. The study area is situated east of the Fokida – Beotia tectonic&lt;br&gt;depression focusing on the relation of the tectonic activity to the formation of the&lt;br&gt;surrounding slopes. As a result of this study, slope formation is related to the two main tectonic phases of the wider area.&lt;/p&gt;</style></abstract></record></records></xml>