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                <gco:CharacterString>An online platform for exploring geothermal energy potential, assessing constraints, and making informed exploration decisions.</gco:CharacterString>
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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:report>
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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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            <gco:CharacterString>The temperature at 100 m was calculated based on Fourier's law of conduction, using the thermal conductivity of the bedrock geology  and the heat flow distribution (Downing &amp; Gray 1986; Lee et al. 1987; Rollin 1995; Barker et al. 2000). The calculated geothermal gradient (average of 26 °C/km) was added to the estimate of the mean annual air temperature, determined from long-term meteorological data, to generate the estimate of temperature at 100 m depth.</gco:CharacterString>
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