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Baltica in the Cordillera?

2011/07/01 by Elizabeth L. Miller, Н. Б. Кузнецов, А. А. Соболева +3 · 2 citations
Earth and Planetary Sciences · #Geological and Geochemical Analysis #High-pressure geophysics and materials #Geological Studies and Exploration #Miller #Library science #Geology #Computer science #Paleontology

paper · doi:10.1130/g31910.1

openalex publication_date 2011/07/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/22

Abstract

Research Article| August 01, 2011 Baltica in the Cordillera? E.L. Miller; E.L. Miller * 1Department of Geology and Environmental Science, Stanford University, Stanford, California 94305, USA *E-mails: [email protected]; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]. Search for other works by this author on: GSW Google Scholar N. Kuznetsov; N. Kuznetsov * 2Geological Institute, Russian Academy of Sciences, Moscow 119017, Russia *E-mails: [email protected]; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]. Search for other works by this author on: GSW Google Scholar A. Soboleva; A. Soboleva * 3Institute of Geology, Komi Scientific Center, Uralian Branch of the Russian Academy of Sciences, Syktyvkar 167982, Russia *E-mails: [email protected]; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]. Search for other works by this author on: GSW Google Scholar O. Udoratina; O. Udoratina * 3Institute of Geology, Komi Scientific Center, Uralian Branch of the Russian Academy of Sciences, Syktyvkar 167982, Russia *E-mails: [email protected]; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]. Search for other works by this author on: GSW Google Scholar M.J. Grove; M.J. Grove * 1Department of Geology and Environmental Science, Stanford University, Stanford, California 94305, USA *E-mails: [email protected]; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]. Search for other works by this author on: GSW Google Scholar G. Gehrels G. Gehrels * 4Department of Geosciences, University of Arizona, Tucson, Arizona 85721, USA *E-mails: [email protected]; [email protected]; [email protected]; [email protected]; [email protected]; [email protected]. Search for other works by this author on: GSW Google Scholar Geology (2011) 39 (8): 791–794. https://doi.org/10.1130/G31910.1 Article history received: 13 Nov 2010 rev-recd: 18 Mar 2011 accepted: 28 Mar 2011 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation E.L. Miller, N. Kuznetsov, A. Soboleva, O. Udoratina, M.J. Grove, G. Gehrels; Baltica in the Cordillera?. Geology 2011;; 39 (8): 791–794. doi: https://doi.org/10.1130/G31910.1 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 U-Pb ages of detrital zircon suites from Paleozoic strata in the Arctic Alaska–Chukotka terrane (AAC), Alexander terrane, northern Sierra terrane, and eastern Klamath terrane of the North American Cordillera suggest an exotic Gondwana or Baltic origin. We evaluate these hypotheses with U-Pb ages of detrital zircon suites from Cambrian–Devonian strata of northern Baltica. Precambrian zircon populations (ca. 0.8–3.0 Ga) from Baltica compare well with similar age detritus in the AAC and Cordilleran terranes, but the amount and age of younger Neoproterozoic and Ordovician–Silurian components are variable. The AAC shares its stratigraphy with Baltica and has the most similar detrital zircon suites. Closing the Arctic places the AAC against the Lomonosov Ridge and the edge of Baltica in pre-Cretaceous time. After the Caledonian orogeny and before the Ural Mountains formed, the Baltica, AAC, and Cordilleran margins shared a Devonian–Carboniferous rift history and became along-strike portions of a Carboniferous–Permian continental margin. This rifting event might have been responsible for the initial separation of Baltica and Caledonian affinity terranes from this margin. 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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