http://earthwise-staging.bgs.ac.uk/index.php?action=history&feed=atom&title=File%3AYGS_CHR_04_DINA_FIG_07.jpgFile:YGS CHR 04 DINA FIG 07.jpg - Revision history2026-04-14T14:07:13ZRevision history for this page on the wikiMediaWiki 1.42.3http://earthwise-staging.bgs.ac.uk/index.php?title=File:YGS_CHR_04_DINA_FIG_07.jpg&diff=41995&oldid=prevScotfot: Scotfot uploaded a new version of File:YGS CHR 04 DINA FIG 07.jpg2019-08-07T19:40:12Z<p>Scotfot uploaded a new version of <a href="/index.php/File:YGS_CHR_04_DINA_FIG_07.jpg" title="File:YGS CHR 04 DINA FIG 07.jpg">File:YGS CHR 04 DINA FIG 07.jpg</a></p>
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</table>Scotfothttp://earthwise-staging.bgs.ac.uk/index.php?title=File:YGS_CHR_04_DINA_FIG_07.jpg&diff=41609&oldid=prevScotfot: User created page with UploadWizard2019-07-31T08:58:52Z<p>User created page with UploadWizard</p>
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{{Information<br />
|description={{en|1=Figure 7 An isochore map of the Scremerston Coal Group and its equivalents. Thicknesses are in metres. The increase in thickness to the south may relate to increasing differential subsidence between the Mid North Sea High and the Southern North Sea Basin. Note the continuing strong differential subsidence between the Alston Block and the Stainmore Trough. The contouring ignores the thick Scremerston facies at well 41/10-1, which is regarded as a facies equivalent of thick Fell Sandstone channel sands in other wells.<br />
{{YGSCarbHydroRes}}}}<br />
|date=2019-07-30 14:15:49<br />
|source=Yorkshire Geological Society<br />
|author=John D. Collinson<br />
|permission=<br />
|other versions=<br />
}}<br />
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