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        <Abstract>Vlaanderen is opgebouwd uit een afwisseling van watervoerende lagen (zand, grind, krijt, vast gesteente, ...) en niet-watervoerende lagen (bijvoorbeeld klei). &#13;
De opeenvolging van deze aquifers en aquitards werd in Vlaanderen gemodelleerd in het hydrogeologisch 3D-model van Vlaanderen (H3Dv2). &#13;
Het hydrogeologisch 3D-model (H3Dv2) werd gemodelleerd op 3 verschillende niveaus van detail: de hoofdeenheden, de subeenheden en de basiseenheden.&#13;
&#13;
Dit rastermodel combineert de verschillende afzonderlijke rasters van het H3Dv2-model in één rasterbestand met in de verschillende banden de basislagen in mTAW van de afzonderlijke hoofd-, sub- en basiseenheden.</Abstract>
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          <Abstract>A sample style for rasters</Abstract>
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        <Abstract>Dit bestand geeft een overzicht van de locatie van de gebruikte seismische lijnen, de campagne waartoe ze behoren, de ouderdom en het doel waarvoor ze gebruikt werden bij de opmaak van het Hydrogeologische 3D model van de Vlaamse ondergrond. Het Hydrogeologisch 3D model is opgemaakt in het kader van de beheersovereenkomst van de Vlaamse overheid met VITO, onder de noemer VLAKO, in opdracht van de Vlaamse Milieumaatschappij</Abstract>
        <KeywordList>
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          <Keyword>VMM</Keyword>
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          <Keyword>H3Dv2</Keyword>
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