Research Article| April 01, 1975 Continuation of the Highland Boundary fault in Ireland M. D. Max; M. D. Max 1Geological Survey of Ireland, 14 Hume Street, Dublin, Ireland Search for other works by this author on: GSW Google Scholar R. P. Riddihough R. P. Riddihough 1Geological Survey of Ireland, 14 Hume Street, Dublin, Ireland Search for other works by this author on: GSW Google Scholar Geology (1975) 3 (4): 206–210. https://doi.org/10.1130/0091-7613(1975)3<206:COTHBF>2.0.CO;2 Article history first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation M. D. Max, R. P. Riddihough; Continuation of the Highland Boundary fault in Ireland. Geology 1975;; 3 (4): 206–210. doi: https://doi.org/10.1130/0091-7613(1975)3<206:COTHBF>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A major geophysical lineament in Ireland is correlated with the Highland Boundary fault in Scotland; it is shown to separate a southern block, deformed in Middle to Late Cambrian time, from a northern block that was deformed in early Ordovician time. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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Max et al. (1975) studied this question.