http://earthwise-staging.bgs.ac.uk/index.php?action=history&feed=atom&title=File%3AGSG_GLA_FIG_26_03.jpg 2026-04-19T04:30:34Z Revision history for this page on the wiki MediaWiki 1.42.3 http://earthwise-staging.bgs.ac.uk/index.php?title=File:GSG_GLA_FIG_26_03.jpg&diff=39632&oldid=prev 2019-02-11T18:34:03Z

<p>User created page with UploadWizard</p> <p><b>New page</b></p><div>=={{int:filedesc}}==<br /> {{Information<br /> |description={{en|1=Figure 26.3. Possible explanation of the metamorphic sole to the ophiolite. A an arc, because of changes in the location and sense of subduction, is driven towards the source of the plate which created it. In colliding with the under-riding plate it underplates onto it the high pressure rocks belonging to this oceanic plate (B). But only fragments of this plate are accreted to the sole of the arc (C).<br /> {{GSGGlasgow}}}}<br /> |date=2019-02-11 18:24:16<br /> |source=Geological Society of Glasgow<br /> |author=Geological Society of Glasgow<br /> |permission=<br /> |other versions=<br /> }}<br /> <br /> =={{int:license-header}}==<br /> {{subst:Custom license marker added by UW}}<br /> {{GSG1}}<br /> <br /> [[Category:Uploaded with UploadWizard]]</div>

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