http://earthwise-staging.bgs.ac.uk/index.php?action=history&feed=atom&title=File%3AYGS_CHR_08_IMAG_FIG_02.jpgFile:YGS CHR 08 IMAG FIG 02.jpg - Revision history2026-04-19T06:01:09ZRevision history for this page on the wikiMediaWiki 1.42.3http://earthwise-staging.bgs.ac.uk/index.php?title=File:YGS_CHR_08_IMAG_FIG_02.jpg&diff=42022&oldid=prevScotfot: User created page with UploadWizard2019-08-11T18:42:45Z<p>User created page with UploadWizard</p>
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|description={{en|1=Figure 2 Location maps showing main structural units, some onshore and SNS Carboniferous reservoirs and the location of the Ollerton case study. Large sandstone bodies are well known across the East Pennine Basin. Although some show a correlation with the underlying structure, such as the Parkgate Rock (Sandstone), which swings round into the Gainsborough Trough, others, such as the sandstones above the Deep Hard, cut across the Dinantian basement.<br />
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{{YGSCarbHydroRes}}}}<br />
|date=2019-08-07 17:44:30<br />
|source=Yorkshire Geological Society<br />
|author=B.A. McGlen and J.H. Rippon<br />
|permission=<br />
|other versions=<br />
}}<br />
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