Example of ensialic ophiolites emplaced in a wrench zone: Innermost Hellenic ophiolite belt (Greek Macedonia)

Research Article| December 01, 1986 Example of ensialic ophiolites emplaced in a wrench zone: Innermost Hellenic ophiolite belt (Greek Macedonia) Jean Bébien; Jean Bébien 1U.A. 735, Laboratoire de Pétrologie, Université de Nancy I, BP 239 F 54506 Vandoeuvre-lès-Nancy Cédex, France Search for other works by this author on: GSW Google Scholar Roland Dubois; Roland Dubois 2Laboratoire de Géologie Historique, Université de Paris-Sud, F 91405 Orsay Cédex, France Search for other works by this author on: GSW Google Scholar Aline Gauthier Aline Gauthier 3U.A. 735, Laboratoire de Pétrologie, Université de Nancy I, BP 239 F 54506 Vandoeuvre-lès-Nancy Cédex, France Search for other works by this author on: GSW Google Scholar Author and Article Information Jean Bébien 1U.A. 735, Laboratoire de Pétrologie, Université de Nancy I, BP 239 F 54506 Vandoeuvre-lès-Nancy Cédex, France Roland Dubois 2Laboratoire de Géologie Historique, Université de Paris-Sud, F 91405 Orsay Cédex, France Aline Gauthier 3U.A. 735, Laboratoire de Pétrologie, Université de Nancy I, BP 239 F 54506 Vandoeuvre-lès-Nancy Cédex, France Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1986) 14 (12): 1016–1019. https://doi.org/10.1130/0091-7613(1986)14<1016:EOEOEI>2.0.CO;2 Article history First Online: 01 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 Jean Bébien, Roland Dubois, Aline Gauthier; Example of ensialic ophiolites emplaced in a wrench zone: Innermost Hellenic ophiolite belt (Greek Macedonia). Geology 1986;; 14 (12): 1016–1019. doi: https://doi.org/10.1130/0091-7613(1986)14<1016:EOEOEI>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 The innermost Hellenic ophiolite belt of northern Greece comprises discontinuous ophiolites of the Guevgueli and Chalkidiki complexes. Field, structural, chemical, and geochronological data indicate that they are broadly autochthonous and were emplaced into continental crust along a northwest-southeast wrench zone during the Middle and Late Jurassic. Variations in structure and petrology along the belt can be related to changes in the tectonics of emplacement from extensional to transcurrent. 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.