Abstract
Research Article| May 01, 2010 Dynamics of deformation and sedimentation in the northern Sierras Pampeanas: An integrated study of the Neogene Fiambalá Basin, NW Argentina: Comment and Discussion Federico M. Dávila Federico M. Dávila † Laboratorio de Análisis de Cuencas, Centro de Investigaciones en Ciencias de la Tierra (CICTERRA-CONICET), Universidad Nacional de Córdoba, Av. V. Sarsfield 1611, Cordoba 5016, Argentina †E-mail: fmdavila@efn.uncor.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Federico M. Dávila † Laboratorio de Análisis de Cuencas, Centro de Investigaciones en Ciencias de la Tierra (CICTERRA-CONICET), Universidad Nacional de Córdoba, Av. V. Sarsfield 1611, Cordoba 5016, Argentina †E-mail: fmdavila@efn.uncor.edu Publisher: Geological Society of America Received: 15 Jul 2009 Accepted: 24 Aug 2009 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 © 2010 Geological Society of America GSA Bulletin (2010) 122 (5-6): 946–949. https://doi.org/10.1130/B30133.1 Article history Received: 15 Jul 2009 Accepted: 24 Aug 2009 First Online: 08 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 Federico M. Dávila; Dynamics of deformation and sedimentation in the northern Sierras Pampeanas: An integrated study of the Neogene Fiambalá Basin, NW Argentina: Comment and Discussion. GSA Bulletin 2010;; 122 (5-6): 946–949. doi: https://doi.org/10.1130/B30133.1 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 SocietyGSA Bulletin Search Advanced Search In a recent contribution to the Geological Society of America Bulletin, Carrapa et al. (2008) provided an interesting geochronological and thermochronological database for the Fiambalá Basin, northern end of the Sierras Pampeanas, which, together with stratigraphic, sedimentological and structural data, led them to interpret a late Miocene–Pliocene foreland reorganization from a simple scenario (e.g., DeCelles and Giles, 1996) to settings dominated by intermontane basement thrusting. They associated this reorganization with the beginning of flat subduction, which would have been coeval (according to Carrapa et al., 2008) with broken foreland stages in the Bermejo Basin (>400 km south).... 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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