Abstract
Research Article| February 01, 1979 Extent and disposition of Grenville tectonism in the Precambrian continental crust adjacent to the North Atlantic M. D. Max M. D. Max 1Irish Geological Survey, 14 Hume Street, Dublin 2, Ireland Search for other works by this author on: GSW Google Scholar Author and Article Information M. D. Max 1Irish Geological Survey, 14 Hume Street, Dublin 2, Ireland Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1979) 7 (2): 76–78. https://doi.org/10.1130/0091-7613(1979)7<76:EADOGT>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; Extent and disposition of Grenville tectonism in the Precambrian continental crust adjacent to the North Atlantic. Geology 1979;; 7 (2): 76–78. doi: https://doi.org/10.1130/0091-7613(1979)7<76:EADOGT>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 Grenville tectonism in the North Atlantic region may have occurred in two main belts. The Grenville province of Canada can be traced into northwest Ireland and France, and the Dalslandian province of Scandinavia can be correlated with the Carolinidian province of northeast Greenland. This configuration would suggest that little wrench faulting (total displacement less than 200 km) has occurred within the Caledonian orogen. 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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