Research Article| November 01, 1985 Evolution of the Yukon-Tanana terrane: Evidence from southeastern Yukon Territory J. K. Mortensen; J. K. Mortensen 1Department of Geological Sciences, University of British Columbia, Vancouver, British Columbia V6T 2B4, Canada Search for other works by this author on: GSW Google Scholar G. A. Jilson G. A. Jilson 2Cyprus Anvil Mining Corporation, 600-1281 West Georgia Street, Vancouver, British Columbia V6E 3K3, Canada Search for other works by this author on: GSW Google Scholar Geology (1985) 13 (11): 806–810. https://doi.org/10.1130/0091-7613(1985)13<806:EOTYTE>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 J. K. Mortensen, G. A. Jilson; Evolution of the Yukon-Tanana terrane: Evidence from southeastern Yukon Territory. Geology 1985;; 13 (11): 806–810. doi: https://doi.org/10.1130/0091-7613(1985)13<806:EOTYTE>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 Yukon-Tanana terrane (YTT) in southeastern Yukon consists predominantly of a mid-Paleozoic volcanic-plutonic (arc?) assemblage built on continental crust. The YTT had experienced strong deformation and metamorphism by Late Triassic time. By mid-Cretaceous the metamorphic complex and Late Triassic clastic rocks derived from it were imbricated with middle and upper Paleozoic "ophiolitic" sheets. The YTT differs markedly from adjacent parts of the North American continental margin in both its depositional and tectonic histories. The composition and tectonic history of the YTT is comparable to that of the Kootenay and Barkerville terranes of southern and central British Columbia from which the YTT may have been displaced. 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.
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