Late Paleozoic radiolarian ages from the Gwydir terrane, New England orogen, eastern Australia

Abstract

Research Article| September 01, 1988 Late Paleozoic radiolarian ages from the Gwydir terrane, New England orogen, eastern Australia Jonathan C. Aitchison Jonathan C. Aitchison 1Department of Geology and Geophysics, University of New England, Armidale, New South Wales 2351, Australia Search for other works by this author on: GSW Google Scholar Author and Article Information Jonathan C. Aitchison 1Department of Geology and Geophysics, University of New England, Armidale, New South Wales 2351, Australia Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1988) 16 (9): 793–795. https://doi.org/10.1130/0091-7613(1988)016<0793:LPRAFT>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 MailTo Tools Icon Tools Get Permissions Search Site Citation Jonathan C. Aitchison; Late Paleozoic radiolarian ages from the Gwydir terrane, New England orogen, eastern Australia. Geology 1988;; 16 (9): 793–795. doi: https://doi.org/10.1130/0091-7613(1988)016<0793:LPRAFT>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 Discoveries of Late Devonian-Early Mississippian Radiolaria in the Gwydir terrane, eastern Australia, indicate that much of the terrane is younger than previously thought. Radiolaria provide valuable constraints on the timing of the development of the Gwydir terrane. Moreover, this new biostratigraphic data indicate that previously published models detailing the development of the New England orogen need to be reappraised. 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.