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• W1990683204 abstract "Research Article| September 01, 1998 Possible crystalline gastroliths of large marine Vertebrata from Oligocene pelitic sediments of the Northern Apennines, Italy Enrico Pandeli; Enrico Pandeli 1Earth Sciences Department, University of Florence, Via La Pira 4, 50121 Florence, Italy Search for other works by this author on: GSW Google Scholar Paola Vannucchi; Paola Vannucchi 2Earth Sciences Department, University of Modena, Piazzale Santa Eufemia 19, 41100 Modena, Italy Search for other works by this author on: GSW Google Scholar Simonetta Monechi Simonetta Monechi 1Earth Sciences Department, University of Florence, Via La Pira 4, 50121 Florence, Italy Search for other works by this author on: GSW Google Scholar Author and Article Information Enrico Pandeli 1Earth Sciences Department, University of Florence, Via La Pira 4, 50121 Florence, Italy Paola Vannucchi 2Earth Sciences Department, University of Modena, Piazzale Santa Eufemia 19, 41100 Modena, Italy Simonetta Monechi 1Earth Sciences Department, University of Florence, Via La Pira 4, 50121 Florence, Italy Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1998) 26 (9): 775–778. https://doi.org/10.1130/0091-7613(1998)026<0775:PCGOLM>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 Enrico Pandeli, Paola Vannucchi, Simonetta Monechi; Possible crystalline gastroliths of large marine Vertebrata from Oligocene pelitic sediments of the Northern Apennines, Italy. Geology 1998;; 26 (9): 775–778. doi: https://doi.org/10.1130/0091-7613(1998)026<0775:PCGOLM>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 Randomly dispersed erratic clasts are found within the pelagic marly-shaly sequences of the Oligocene Scisti Varicolori Formation (Cervarola-Falterona unit of the Tuscan domain). These clasts are centimeters to decimeters in size and subrounded to well rounded; their shape suggests an origin in a fluvial and partly littoral environment. The clasts are composed of low- to medium-grade metamorphic rocks, andesitic volcanic rocks, and Late Jurassic–Early Cretaceous pelagic limestones. The source area of the crystalline material is interpreted to be the central-western sector of the Alpine chain or the Corsica-Sardinia area. In addition, the peculiar surfaces of these clasts, as well as their isolated occurrence in the pelagic shales of the Scisti Varicolori, suggest an uncommon depositional mechanism, such as redeposited gastroliths of large marine Vertebrata. 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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• W1990683204 title "Possible crystalline gastroliths of large marine Vertebrata from Oligocene pelitic sediments of the Northern Apennines, Italy" @default.
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