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• W2138967333 abstract "Research Article| June 01, 1989 Evidence of a late Mesozoic ocean basin and subduction-accretion in the southern Greek Neo-Tethys Peter D. Clift; Peter D. Clift 1Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, Scotland Search for other works by this author on: GSW Google Scholar Alastair H. F. Robertson Alastair H. F. Robertson 1Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, Scotland Search for other works by this author on: GSW Google Scholar Author and Article Information Peter D. Clift 1Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, Scotland Alastair H. F. Robertson 1Grant Institute of Geology, University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, Scotland Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1989) 17 (6): 559–563. https://doi.org/10.1130/0091-7613(1989)017<0559:EOALMO>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 Peter D. Clift, Alastair H. F. Robertson; Evidence of a late Mesozoic ocean basin and subduction-accretion in the southern Greek Neo-Tethys. Geology 1989;; 17 (6): 559–563. doi: https://doi.org/10.1130/0091-7613(1989)017<0559:EOALMO>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 Ermioni Complex in the east of the Argolis Peninsula (Adheres), Peloponnesus, comprises a tectonically thickened (10-15 km) wedge of terrigenous, early Tertiary (Paleocene-Eocene) flysch, interleaved with thin, tectonically disrupted sheets of basic lava, massive sulfides, and metalliferous and pelagic sediments. Immobile trace-element analysis of the basalts in the Ermioni Complex suggests an oceanic, mid-ocean ridge, and/or subduction-related origin. The planktonic foraminifer Globotruncanita elevata in pelagic limestones depositionally overlying the basalts is Campanian-Maastrichtian in age. We propose that the basaltic slices represent fragments of a Neo-Tethyan ocean of Late Cretaceous age in the southern Greece area. The basin subsequently closed in the early Tertiary (Paleocene-Eocene), with trench-type Flysch accumulation and accretion of oceanic lava slices. The new evidence contradicts the current view that the Neo-Tethys was fully sutured by Early Cretaceous time in this area. 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." @default.
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• W2138967333 title "Evidence of a late Mesozoic ocean basin and subduction-accretion in the southern Greek Neo-Tethys" @default.
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