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                    <gco:CharacterString>INSPIRE Implementing rules laying down technical arrangements for the interoperability and harmonisation of Geology</gco:CharacterString>
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                        <gco:Date>2011</gco:Date>
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                        <gmd:CI_DateTypeCode codeList="https://schemas.isotc211.org/schemas/19139/resources/codelist/gmxCodelists.xml#CI_DateTypeCode" codeListValue="publication">publication</gmd:CI_DateTypeCode>
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                <gco:CharacterString>See the referenced specification</gco:CharacterString>
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                <gco:Boolean>false</gco:Boolean>
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        </gmd:DQ_DomainConsistency>
      </gmd:report>
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                <gmd:CI_Citation>
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                    <gco:CharacterString>Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services</gco:CharacterString>
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                      <gmd:date>
                        <gco:Date>2010-12-08</gco:Date>
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                      <gmd:dateType>
                        <gmd:CI_DateTypeCode codeList="https://schemas.isotc211.org/schemas/19139/resources/codelist/gmxCodelists.xml#CI_DateTypeCode" codeListValue="publication">publication</gmd:CI_DateTypeCode>
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                <gco:Boolean>false</gco:Boolean>
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            <gco:CharacterString>Samples with reliable characteristic remanent directions were analysed using palaeomagnetic, rock-magnetic, microscopy and paleointensity methods. Bourinot samples were studied using thermal Thellier experiments with the IZZI+ protocol. Itabaiana samples were analysed using thermal and microwave Thellier, modified Shaw, and continuous Triaxe/Wilson methods. Hysteresis, thermomagnetic magnetisation and susceptibility measurements, scanning electron microscopy and EDX were used to characterise remanence carriers and thermal stability. Thellier-type results were screened using SCOPE, while other results were assessed using method-specific reliability criteria. Only sites consistent with established primary palaeomagnetic populations were retained.</gco:CharacterString>
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