http://earthwise-staging.bgs.ac.uk/index.php?action=history&feed=atom&title=File%3AP915421.png 2026-04-23T07:21:21Z Revision history for this page on the wiki MediaWiki 1.42.3 http://earthwise-staging.bgs.ac.uk/index.php?title=File:P915421.png&diff=16961&oldid=prev 2015-07-10T18:43:34Z

<p>User created page with UploadWizard</p> <p><b>New page</b></p><div>=={{int:filedesc}}==<br /> {{Information<br /> |description={{en|1=Geological sketch map and section of the Jura area—with along-strike stratigraphical section showing relationships at the end of Craignish Phyllite times (modified from Anderton, 1979; 1985). STF—Scarba Transfer Fault and ITF—Islay Transfer Fault are interpreted growth faults and do not crop out at the surface. Note that the sense of movement on the STF reverses after the deposition of the Jura Quartzite. Hence the thick accumulation of Jura Quartzite lies to the south of the fault, whereas the thick accumulation of Easdale Slate and Craignish Phyllite lies to the north. BD = Bonahaven Dolomite; PAT = Port Askaig Tillite. From: Figure 13 in Stephenson, D, and Gould, D. 1995. British regional geology: Grampian Highlands. Fourth edition. Keyworth, Nottingham: British Geological Survey.}}<br /> |date=2015-07-10 19:39:49<br /> |source=British Geological Survey<br /> |author=British Geological Survey<br /> |permission=<br /> |other versions=<br /> }}<br /> <br /> =={{int:license-header}}==<br /> {{subst:Custom license marker added by UW}}<br /> {{BGS}}<br /> <br /> [[Category:Uploaded with UploadWizard]]</div>

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