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- W1976564237 abstract "Research Article| August 01, 1997 Early Paleozoic paleogeography of Laurentia and western Gondwana: Evidence from tectonic subsidence analysis Kenneth E. Williams Kenneth E. Williams 1Texaco Inc., Exploration and Production Technology Department, 3901 Briarpark, Houston, Texas 77042 Search for other works by this author on: GSW Google Scholar Geology (1997) 25 (8): 747–750. https://doi.org/10.1130/0091-7613(1997)025<0747:EPPOLA>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 Kenneth E. Williams; Early Paleozoic paleogeography of Laurentia and western Gondwana: Evidence from tectonic subsidence analysis. Geology 1997;; 25 (8): 747–750. doi: https://doi.org/10.1130/0091-7613(1997)025<0747:EPPOLA>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 A number of terranes were present in the early Paleozoic ocean between Laurentia and Gondwana following rifting. The precise location of these microcontinents and island arcs is unclear. We present tectonic subsidence curves from selected basins that may provide some constraints on the possible paleogeographic interpretations for this time interval. Among these tectonic blocks were the Precordillera terrane that originated in the Ouachita area of Laurentia and the composite Avalon-Carolina terrane that was derived from the Gondwana margin. Also present were the island-arc terranes of Famatina, Mixteca, and Zapoteca. The Precordillera and Famatina terranes are currently located in southern South America. The Avalon-Carolina terrane is in eastern North America. The Mixteca and Zapoteca terranes are in Central America. A review of previous work augmented by new tectonic subsidence analysis indicates that these terranes were swept up by early Paleozoic plate movements and were translated to approximately their present relative positions by the Early Carboniferous. 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." @default.
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- W1976564237 title "Early Paleozoic paleogeography of Laurentia and western Gondwana: Evidence from tectonic subsidence analysis" @default.
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