Overthrust terranes in the Lachlan fold belt, southeastern Australia

Research Article| June 01, 1986 Overthrust terranes in the Lachlan fold belt, southeastern Australia Christopher L. Fergusson; Christopher L. Fergusson 1Department of Earth Sciences, Monash University, Clayton, Victoria 3168, Australia Search for other works by this author on: GSW Google Scholar David R. Gray; David R. Gray 1Department of Earth Sciences, Monash University, Clayton, Victoria 3168, Australia Search for other works by this author on: GSW Google Scholar Ray A.F. Cas Ray A.F. Cas 1Department of Earth Sciences, Monash University, Clayton, Victoria 3168, Australia Search for other works by this author on: GSW Google Scholar Geology (1986) 14 (6): 519–522. https://doi.org/10.1130/0091-7613(1986)14<519:OTITLF>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 Christopher L. Fergusson, David R. Gray, Ray A.F. Cas; Overthrust terranes in the Lachlan fold belt, southeastern Australia. Geology 1986;; 14 (6): 519–522. doi: https://doi.org/10.1130/0091-7613(1986)14<519:OTITLF>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 Paleozoic history of the Lachlan fold belt involves terrane translation and accretion of discrete allochthonous fragments. Four major terranes developed adjacent to the Gondwana continental margin and were overthrust in the Middle Devonian to form a partly composite crust for southeastern Australia. 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.