<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-06-28T20:41:10Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/33602" metadataPrefix="qdc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/33602</identifier><datestamp>2026-01-28T13:23:16Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</setSpec></header><metadata><qdc:qualifieddc xmlns:qdc="http://dspace.org/qualifieddc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://purl.org/dc/elements/1.1/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dc.xsd http://purl.org/dc/terms/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dcterms.xsd http://dspace.org/qualifieddc/ http://www.ukoln.ac.uk/metadata/dcmi/xmlschema/qualifieddc.xsd">
   <dc:title>Analysis of co-located measurements made with a LaCoste&amp;Romberg Graviton-EG gravimeter and two superconducting gravimeters at Strasbourg (France) and Yebes (Spain)</dc:title>
   <dc:creator>Arnoso, J.</dc:creator>
   <dc:creator>Riccardi, U.</dc:creator>
   <dc:creator>Hinderer, J.</dc:creator>
   <dc:creator>Cordoba, B.</dc:creator>
   <dc:creator>González Montesinos, Fuensanta</dc:creator>
   <dcterms:abstract>Two experiments of intercomparison between the LaCoste&amp;Romberg Graviton-EG1194 spring gravimeter and the superconducting gravimeters SG-026 and OSG-064, operating respectively at J9-Strasbourg (France) and CDT-Yebes (Spain), were analyzed. The main objective was to check the instrumental response of the spring meter, both in amplitude and phase as well as its time stability. A general conclusion is that normalization factors have been obtained with a similar ratio for main diurnal constituent O1 at both observing sites. The accuracy of scale factors was determined at the level of 0.03 % (at J9-Strasbourg) and 0.1 % (at CDT-Yebes). For the semidiurnal constituent M2, slight differences were found at J9-Strasbourg, which would require further investigations. Site effects were also demonstrated by considering the different response of the spring gravimeter to tilts and atmospheric pressure variations at both sites.</dcterms:abstract>
   <dcterms:dateAccepted>2023-06-19T13:24:52Z</dcterms:dateAccepted>
   <dcterms:available>2023-06-19T13:24:52Z</dcterms:available>
   <dcterms:created>2023-06-19T13:24:52Z</dcterms:created>
   <dcterms:issued>2014</dcterms:issued>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/33602</dc:identifier>
   <dc:identifier>2213-5812</dc:identifier>
   <dc:identifier>10.1007/s40328-014-0043-y</dc:identifier>
   <dc:relation>CGL2011-25494</dc:relation>
   <dc:relation>GR35/10-A</dc:relation>
   <dc:rights>metadata only access</dc:rights>
   <dc:publisher>Springer</dc:publisher>
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