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The geochemistry of a rock unit, and its trace element signature, in particular, is an important factor in determining its origin. Many trace elements are hosted in scarce, fine-grained minerals in the rocks, e.g. apatite, zircon and monazite. These minerals are resistant to weathering with the effect that their abundance is upgraded in the stream sediments relative to their abundance in the source rocks. Again, because the stream sediment data cover regions with little or no geochemical data on rocks, the stream sediment chemical maps may assist in identifying rock complexes of a certain origin.</gco:CharacterString>
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                     <gmd:pass>
                        <gco:Boolean>false</gco:Boolean>
                     </gmd:pass>
                  </gmd:DQ_ConformanceResult>
               </gmd:result>
            </gmd:DQ_DomainConsistency>
         </gmd:report>
         <gmd:lineage>
            <gmd:LI_Lineage>
               <gmd:statement>
                  <gco:CharacterString>Data are based on https://data.geus.dk/geonetwork/srv/eng/catalog.search#/metadata/8abf8aef-e244-4f70-9c48-a455cf4c32ae</gco:CharacterString>
               </gmd:statement>
            </gmd:LI_Lineage>
         </gmd:lineage>
      </gmd:DQ_DataQuality>
  </gmd:dataQualityInfo>
</gmd:MD_Metadata>