<?xml version="1.0" encoding="UTF-8"?><resource xmlns="http://datacite.org/schema/kernel-4" xmlns:mcrmods="http://www.mycore.de/xslt/mods" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.3/metadata.xsd"><identifier identifierType="DOI">10.57892/100-343</identifier><creators><creator><creatorName nameType="Personal">Wilken, Dennis</creatorName><givenName>Dennis</givenName><familyName>Wilken</familyName><nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org/">0000-0002-5128-351X</nameIdentifier></creator><creator><creatorName nameType="Personal">Vött, Andreas</creatorName><givenName>Andreas</givenName><familyName>Vött</familyName><nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org/">0000-0001-7001-6225</nameIdentifier></creator><creator><creatorName nameType="Personal">Wilken, Dennis</creatorName><givenName>Dennis</givenName><familyName>Wilken</familyName><nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org/">0000-0002-5128-351X</nameIdentifier></creator></creators><titles><title>Geophysical prospection data at the archaeological site of Kleidi/Samikon (Greece)</title></titles><publisher>Kiel University</publisher><publicationYear>2026</publicationYear><subjects><subject subjectScheme="sdnb">550</subject></subjects><contributors><contributor contributorType="HostingInstitution"><contributorName nameType="Organizational">Kiel University</contributorName></contributor><contributor contributorType="Other"><contributorName nameType="Personal">Fischer, Peter</contributorName><givenName>Peter</givenName><familyName>Fischer</familyName><nameIdentifier nameIdentifierScheme="ORCID" schemeURI="http://orcid.org/">0000-0002-8410-5824</nameIdentifier></contributor></contributors><dates><date dateType="Issued">2026-03-26</date></dates><language>en</language><resourceType resourceTypeGeneral="Dataset">research_data</resourceType><alternateIdentifiers><alternateIdentifier alternateIdentifierType="URL">https://opendata.uni-kiel.de/receive/fdr_mods_00000343</alternateIdentifier><alternateIdentifier alternateIdentifierType="MyCoRe">fdr_mods_00000343</alternateIdentifier></alternateIdentifiers><relatedIdentifiers><relatedIdentifier relatedIdentifierType="URL" relationType="HasMetadata" relatedMetadataScheme="mods" schemeURI="https://www.loc.gov/standards/mods/v3/mods-3-7.xsd">https://opendata.uni-kiel.de/receive/fdr_mods_00000343?XSL.Transformer=mods</relatedIdentifier></relatedIdentifiers><rightsList><rights xml:lang="en" rightsURI="https://creativecommons.org/licenses/by/4.0/" rightsIdentifier="CC-BY-4.0">Attribution 4.0</rights></rightsList><descriptions><description descriptionType="Abstract">The present dataset comprises three different geophysical methods that were performed in 2021 and 2023 at Kleidi/Samikon ( 21.59224°E ,37.53001°N) in the Framework of a geoarchaeological research project searching for the ancient sanctuary of Poseidon at the site. Datasets are: Frequency domain electromagnetic induction (CMD-Explorer by GF-instruments, in HCP mode, carried 1m above surface, 10Hz sampling, RTK-DGPS data was collected using a Stonex S9i). The data is available as processed, binned geotiff EPSG 32634 (cond1-cond3 and IP4-IP6 referring to quadrature(apparent conductivity) and inphase component of the increasing coil distances). The binned dataset was inverted for each bin in 1D resulting in a pseudo 3D cube, saved as standard vtk-file. Raw data is provided as ascii-file (.dat files) Magnetic Gradiometry data using an array of six Foerster Fluxgate gradiometers (sampling 20Hz), positioning with Stonex S9i RTK-DGPS. The data is provided as binned geotiff EPSG 32634 Electrical resistivity tomography profile SAM ERT 17, measured with a syscal R1+switch 48, with 48 electrodes. Measurements were done in Wenner‐Schlumberger configuration. The subsequent least squares inversion was accomplished using the RES2DINV (Loke and Barker (1996)) software, involving iterations until a final absolute error of 2.2 Ωm. For the inversion, an initial damping factor of 0.1 and a minimum damping factor of 0.03 was used. The root mean square (RMS) convergence limit was set to 5 %. Data is provided as .INV ascii format comprising electrode positions and elevations on profile and apparent resistivity values. Absolute electrode positions are attached as shape-file (ERT17.shp).</description></descriptions></resource>