http://earthwise-staging.bgs.ac.uk/index.php?action=history&feed=atom&title=File%3AP915469.jpg 2026-04-23T20:23:19Z Revision history for this page on the wiki MediaWiki 1.42.3 http://earthwise-staging.bgs.ac.uk/index.php?title=File:P915469.jpg&diff=19016&oldid=prev 2015-07-20T16:57:06Z

<p>User created page with UploadWizard</p> <p><b>New page</b></p><div>=={{int:filedesc}}==<br /> {{Information<br /> |description={{en|1=Balanced cross-sections through the Moine Thrust Zone. a Through the Dundonnell Antiform perpendicular to its axis and oblique to the direction of thrusting; the partially restored section above shows the position of the units prior to thrust formation (from Elliot and Johnson, 1980) b Through the imbricated Cambro-Ordovician sequence below the Arnaboll Thrust, ESE of Loch Eriboll (modified after Coward and Kim, 1981); the section is parallel to the direction of thrusting C Across the southern part of the Assynt Window, showing the Ben More and Moine Thrusts. Note that the present upper levels of the thrust zone (formerly deeper crustal levels) contain recumbently folded Lewisian gneiss and Torridonian sandstone (modified after Elliot and Johnson, 1980) . From: Figure 12 . Johnstone, G S and Mykura, W. 1989. British regional geology: Northern Highlands of Scotland. Fourth edition. Keyworth, Nottingham: British Geological Survey.}}<br /> |date=2015-07-16 17:43:33<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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