<?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%">Giannopoulos, I.K.</style></author><author><style face="normal" font="default" size="100%">Alexopoulos, J.D.</style></author><author><style face="normal" font="default" size="100%">Mitsika, G.S.</style></author><author><style face="normal" font="default" size="100%">Konsolaki, A.</style></author><author><style face="normal" font="default" size="100%">Dilalos, S.</style></author><author><style face="normal" font="default" size="100%">Vassilakis, E</style></author><author><style face="normal" font="default" size="100%">Voulgaris, N.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A Preliminary Geophysical Investigation Regarding the Possible Extension of Alistrati Cave in Serres Greece</style></title><secondary-title><style face="normal" font="default" size="100%">Near Surface Geoscience 2023 - 29th European Meeting of Environmental and Engineering Geophysics</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2023</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.earthdoc.org/content/papers/10.3997/2214-4609.202320045</style></url></web-urls></urls><number><style face="normal" font="default" size="100%">1</style></number><publisher><style face="normal" font="default" size="100%">European Association of Geoscientists &amp;amp; Engineers</style></publisher><pub-location><style face="normal" font="default" size="100%">Edinburg, UK</style></pub-location><volume><style face="normal" font="default" size="100%">2023</style></volume><pages><style face="normal" font="default" size="100%">5</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The cave of Alistrati, is located in the Prefecture of Serres, Northern Greece near the foothills of&lt;br&gt;Mount Menoikio, in the area of Petroto. This area is structured by crystalline limestones, where the&lt;br&gt;development of a complex and multilevel karst system is favored. An extensive geomorphological&lt;br&gt;survey was carried out for the accurate mapping of the karst surface above the cave, using UAS. For&lt;br&gt;the investigation of a possible lateral extension of the existing karstic conduit, a detailed surface&lt;br&gt;geophysical investigation was carried out. More specifically, three geophysical techniques were&lt;br&gt;implemented: a) the Electrical Resistivity Tomography (ERT), b) the Ground Penetrating Radar&lt;br&gt;(GPR) technique and c) the Very-Low Frequency (VLF) method. These 13 lines of the three&lt;br&gt;geophysical techniques are fully matched at 4 locations and were join-interpreted, yielding remarkable&lt;br&gt;findings. The comparative results of the above geophysical techniques, as well as their 3D&lt;br&gt;presentation, highlight similar geophysical anomalies, evaluated as different types of karst system&lt;br&gt;structures. Therefore, the combined geophysical survey has indicated the existence and&lt;br&gt;interconnection of the first two karst levels of the area, up to a depth of 50m, as well as the possible&lt;br&gt;extension of the Alistrati karstic conduit to the northeast.&lt;/p&gt;</style></abstract></record></records></xml>