http://earthwise-staging.bgs.ac.uk/index.php?action=history&feed=atom&title=OR%2F12%2F023_Results
OR/12/023 Results - Revision history
2026-04-19T08:08:49Z
Revision history for this page on the wiki
MediaWiki 1.42.3
http://earthwise-staging.bgs.ac.uk/index.php?title=OR/12/023_Results&diff=44862&oldid=prev
Dbk at 12:12, 18 December 2019
2019-12-18T12:12:54Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:12, 18 December 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The starting material has previously been analysed and the results reported by West et al., (2011)<ref name="West 2011">WEST, J M, MCKINLEY, I G, PALUMBO-ROE, B, and ROCHELLE, C A. 2011. Potential impact of CO2 storage on</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The starting material has previously been analysed and the results reported by West et al., (2011)<ref name="West 2011">WEST, J M, MCKINLEY, I G, PALUMBO-ROE, B, and ROCHELLE, C A. 2011. Potential impact of CO2 storage on</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>subsurface microbial ecosystems and implication for groundwater quality. Energy Procedia, 4, 3163–3170. [doi:10.1016/j.egypro.2011.02.231].</ref>. In summary, the sample comprises of major amounts of quartz, minor amounts of feldspars (K-feldspar and plagioclase) and ‘mica’ (undifferentiated mica species possibly including muscovite, biotite, illite, illite/smectite etc) and trace amounts of chlorite and hematite. The clay fraction (<2 μm) is composed of illite, illite-smectite mixed-layer clay and chlorite.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>subsurface microbial ecosystems and implication for groundwater quality. Energy Procedia, 4, 3163–3170. <ins style="font-weight: bold; text-decoration: none;">[</ins>[doi:10.1016/j.egypro.2011.02.231<ins style="font-weight: bold; text-decoration: none;">]</ins>].</ref>. In summary, the sample comprises of major amounts of quartz, minor amounts of feldspars (K-feldspar and plagioclase) and ‘mica’ (undifferentiated mica species possibly including muscovite, biotite, illite, illite/smectite etc) and trace amounts of chlorite and hematite. The clay fraction (<2 μm) is composed of illite, illite-smectite mixed-layer clay and chlorite.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Characteristics of the post-experimental materials==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Characteristics of the post-experimental materials==</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Whole rock mineralogical analysis results===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Whole rock mineralogical analysis results===</div></td></tr>
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Dbk
http://earthwise-staging.bgs.ac.uk/index.php?title=OR/12/023_Results&diff=44861&oldid=prev
Dbk at 12:12, 18 December 2019
2019-12-18T12:12:37Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:12, 18 December 2019</td>
</tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l5">Line 5:</td>
<td colspan="2" class="diff-lineno">Line 5:</td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The starting material has previously been analysed and the results reported by West et al., (2011)<ref name="West 2011">WEST, J M, MCKINLEY, I G, PALUMBO-ROE, B, and ROCHELLE, C A. 2011. Potential impact of CO2 storage on</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The starting material has previously been analysed and the results reported by West et al., (2011)<ref name="West 2011">WEST, J M, MCKINLEY, I G, PALUMBO-ROE, B, and ROCHELLE, C A. 2011. Potential impact of CO2 storage on</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>subsurface microbial ecosystems and implication for groundwater quality. Energy Procedia, 4, 3163–3170. doi:10.1016/j.egypro.2011.02.231.</ref>. In summary, the sample comprises of major amounts of quartz, minor amounts of feldspars (K-feldspar and plagioclase) and ‘mica’ (undifferentiated mica species possibly including muscovite, biotite, illite, illite/smectite etc) and trace amounts of chlorite and hematite. The clay fraction (<2 μm) is composed of illite, illite-smectite mixed-layer clay and chlorite.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>subsurface microbial ecosystems and implication for groundwater quality. Energy Procedia, 4, 3163–3170. <ins style="font-weight: bold; text-decoration: none;">[</ins>doi:10.1016/j.egypro.2011.02.231<ins style="font-weight: bold; text-decoration: none;">]</ins>.</ref>. In summary, the sample comprises of major amounts of quartz, minor amounts of feldspars (K-feldspar and plagioclase) and ‘mica’ (undifferentiated mica species possibly including muscovite, biotite, illite, illite/smectite etc) and trace amounts of chlorite and hematite. The clay fraction (<2 μm) is composed of illite, illite-smectite mixed-layer clay and chlorite.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Characteristics of the post-experimental materials==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Characteristics of the post-experimental materials==</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Whole rock mineralogical analysis results===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Whole rock mineralogical analysis results===</div></td></tr>
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Dbk
http://earthwise-staging.bgs.ac.uk/index.php?title=OR/12/023_Results&diff=40967&oldid=prev
Dbk: 1 revision imported
2019-05-28T14:01:24Z
<p>1 revision imported</p>
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<td colspan="1" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 15:01, 28 May 2019</td>
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Dbk
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Ajhil: /* Tungsten */
2019-05-16T14:39:59Z
<p><span dir="auto"><span class="autocomment">Tungsten</span></span></p>
<a href="http://earthwise-staging.bgs.ac.uk/index.php?title=OR/12/023_Results&diff=40966">Show changes</a>
Ajhil