<efrbr:recordSet xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:efrbr="http://vfrbr.info/efrbr/1.1" xmlns:efrbr-work="http://vfrbr.info/efrbr/1.1/work" xmlns:efrbr-expression="http://vfrbr.info/efrbr/1.1/expression" xmlns:efrbr-manifestation="http://vfrbr.info/efrbr/1.1/manifestation" xmlns:efrbr-person="http://vfrbr.info/efrbr/1.1/person" xmlns:efrbr-corporateBody="http://vfrbr.info/efrbr/1.1/corporateBody" xmlns:efrbr-concept="http://vfrbr.info/efrbr/1.1/concept" xmlns:efrbr-structure="http://vfrbr.info/efrbr/1.1/structure" xmlns:efrbr-responsible="http://vfrbr.info/efrbr/1.1/responsible" xmlns:efrbr-subject="http://vfrbr.info/efrbr/1.1/subject" xmlns:efrbr-other="http://vfrbr.info/efrbr/1.1/other" xsi:schemaLocation="http://vfrbr.info/efrbr/1.1 http://vfrbr.info/schemas/1.1/efrbr.xsd"><efrbr:entities><efrbr-work:work identifier="http://purl.tuc.gr/dl/dias/F0EB5546-C66C-454C-AFFB-AE2BBDAAD5A6"><efrbr-work:titleOfTheWork>Geophysical survey at the Omalos Plateau, Chania, Crete</efrbr-work:titleOfTheWork></efrbr-work:work><efrbr-expression:expression identifier="http://purl.tuc.gr/dl/dias/F0EB5546-C66C-454C-AFFB-AE2BBDAAD5A6"><efrbr-expression:titleOfTheExpression>Geophysical survey at the Omalos Plateau, Chania, Crete</efrbr-expression:titleOfTheExpression><efrbr-expression:formOfExpression vocabulary="DIAS:TYPES">
            Peer-Reviewed Journal Publication
            Δημοσίευση σε Περιοδικό με Κριτές
         </efrbr-expression:formOfExpression><efrbr-expression:dateOfExpression type="issued">2015-11-10</efrbr-expression:dateOfExpression><efrbr-expression:dateOfExpression type="published">2004</efrbr-expression:dateOfExpression><efrbr-expression:languageOfExpression vocabulary="iso639-1">el</efrbr-expression:languageOfExpression><efrbr-expression:summarizationOfContent>This paper discusses the preliminary results of a geophysical survey that was carried out at the Omalos plateau in Chania, Crete. The geophysical survey included measurements of electrical tomography, electrical mapping, seismic refraction, georadar, VLF and gravity. The aim of this survey is to compare the results from different geophysical methods used in imaging dolines and karstic features. The processing of the measurements indicates three geoelectrical layers. The first layer of extremely high electrical resistivity is attributed to alluvial – dilluvial deposits. The second layer of very low electrical resistivity reflects mainly the presence of marls. Finally, the third geoelectrical layer outlines the carbonate bedrock, whose relief appears highly irregular. The comparison of all geophysical methods leads to the same results, concerning the detection of dolines and karstic anomalies at the Omalos plateau. </efrbr-expression:summarizationOfContent><efrbr-expression:useRestrictionsOnTheExpression type="creative-commons">http://creativecommons.org/licenses/by/4.0/</efrbr-expression:useRestrictionsOnTheExpression><efrbr-expression:note type="journal name">Bulletin of the Geological Society of Greece</efrbr-expression:note><efrbr-expression:note type="journal number">3</efrbr-expression:note><efrbr-expression:note type="page range">1204-1213</efrbr-expression:note></efrbr-expression:expression><efrbr-person:person identifier="C4E2E5AD-9AB6-4D8D-8E93-6BF4A3F4B05D"><efrbr-person:nameOfPerson vocabulary="">
             Vafidis Αntonis
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            Manoutsoglou M.
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            Andronikidis Νikos
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            Koukadaki Μ.
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            Hamdan Ali-Hamdan
            Hamdan Hamdan
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            Kritikakis Georgios
            Κρητικακης Γεωργιος
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            Oikonomou Nikolaos
            Οικονομου Νικολαος
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            Spanoudakis Nikolaos
            Σπανουδακης Νικολαος
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            Geophysical imaging systems
            imaging systems in geophysics
            geophysical imaging systems
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