Title: Is the Taconian orogeny of southern Quebec the result of an Oman-type obduction?
Abstract:Research Article| February 01, 1995 Is the Taconian orogeny of southern Quebec the result of an Oman-type obduction? Nicolas Pinet; Nicolas Pinet 1Institut National de la Recherche Scientifique-Geores...Research Article| February 01, 1995 Is the Taconian orogeny of southern Quebec the result of an Oman-type obduction? Nicolas Pinet; Nicolas Pinet 1Institut National de la Recherche Scientifique-Georessources, Case postale 7500, Sainte-Foy, Quebec G1V 4C7, Canada Search for other works by this author on: GSW Google Scholar Alain Tremblay Alain Tremblay 1Institut National de la Recherche Scientifique-Georessources, Case postale 7500, Sainte-Foy, Quebec G1V 4C7, Canada Search for other works by this author on: GSW Google Scholar Author and Article Information Nicolas Pinet 1Institut National de la Recherche Scientifique-Georessources, Case postale 7500, Sainte-Foy, Quebec G1V 4C7, Canada Alain Tremblay 1Institut National de la Recherche Scientifique-Georessources, Case postale 7500, Sainte-Foy, Quebec G1V 4C7, Canada Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1995) 23 (2): 121–124. https://doi.org/10.1130/0091-7613(1995)023<0121:ITTOOS>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Nicolas Pinet, Alain Tremblay; Is the Taconian orogeny of southern Quebec the result of an Oman-type obduction?. Geology 1995;; 23 (2): 121–124. doi: https://doi.org/10.1130/0091-7613(1995)023<0121:ITTOOS>2.3.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 The Taconian orogeny is generally considered to have resulted from an arc-continent collision. However, geochronological data indicate that much Taconian deformation predates arc magmatism. We propose that the Late Ordovician–Early Silurian tectonic environment in southern Quebec resembled the configuration of the Oman-Iran transect, where subduction took place in the final stage of a large obduction. 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.Read More
Publication Year: 1995
Publication Date: 1995-01-01
Language: en
Type: article
Indexed In: ['crossref']
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Cited By Count: 18
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