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                <gco:Boolean>false</gco:Boolean>
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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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                        <gco:Date>2010-12-08</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 http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF</gco:CharacterString>
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                <gco:Boolean>false</gco:Boolean>
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            <gco:CharacterString>Rocks were imaged with X-ray microtomography scanners: Nikon XTH225ST (University of Bristol) or GE Phoenix v|tome|x M 240/180kV Dual Tube µCT (Smithsonian Institution, USA). Image stacks were processed using Avizo software to segment the phenocrysts phases, groundmass and pores. Phenocrystals and microcrystals of the same mineral phase are separated using Top-Hat technique. The outcome of the 3D segmentation is a label file with one layer per class (e.g. pores). Binary images were generated separating the palaeo-porosity (groundmass+pores) and the phenocrysts. An axis connectivity analysis separates the connected- from isolated palaeo-pores. The outcome of a permeability simulation through the connected palaeo-porosity is a vector matrix. Electron microprobe analyses of plagioclase and amphibole phenocrysts of three Saint Kitts samples were conducted with a JEOL JXA8530F EPMA.</gco:CharacterString>
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        </gmd:LI_Lineage>
      </gmd:lineage>
    </gmd:DQ_DataQuality>
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