Upper Cretaceous–Paleocene magnetic stratigraphy at Gubbio, Italy IV. Upper Maastrichtian-Paleocene Magnetic Stratigraphy

Research Article| March 01, 1977 Upper Cretaceous–Paleocene magnetic stratigraphy at Gubbio, Italy IV. Upper Maastrichtian-Paleocene Magnetic Stratigraphy WILLIAM M. ROGGENTHEN; WILLIAM M. ROGGENTHEN 1Department of Geological and Geophysical Sciences, Princeton University, Princeton, New Jersey 08540 Search for other works by this author on: GSW Google Scholar GIOVANNI NAPOLEONE GIOVANNI NAPOLEONE 2Istituto di Geologia e Paleontologia, Via lamarmoro, 4, Florence, Italy Search for other works by this author on: GSW Google Scholar Author and Article Information WILLIAM M. ROGGENTHEN 1Department of Geological and Geophysical Sciences, Princeton University, Princeton, New Jersey 08540 GIOVANNI NAPOLEONE 2Istituto di Geologia e Paleontologia, Via lamarmoro, 4, Florence, Italy Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1977) 88 (3): 378–382. https://doi.org/10.1130/0016-7606(1977)88<378:UCMSAG>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 Email Permissions Search Site Citation WILLIAM M. ROGGENTHEN, GIOVANNI NAPOLEONE; Upper Cretaceous–Paleocene magnetic stratigraphy at Gubbio, Italy IV. Upper Maastrichtian-Paleocene Magnetic Stratigraphy. GSA Bulletin 1977;; 88 (3): 378–382. doi: https://doi.org/10.1130/0016-7606(1977)88<378:UCMSAG>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 SocietyGSA Bulletin Search Advanced Search Abstract Pelagic limestones ranging in age from mid-Maastrichtian through Paleocene yield several well-defined magnetic polarity zones. These zones are tied to the planktic foraminiferal zonation at this site and are correlated with magnetic anomalies 26 through 31. 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.