How does the Nazca Ridge subduction influence the modern Amazonian foreland basin?
2007; Geological Society of America; Volume: 35; Issue: 6 Linguagem: Inglês
10.1130/g23237a.1
ISSN1943-2682
AutoresNicolás Espurt, Patrice Baby, Stéphane Brusset, Martín Roddaz, Wilber Hermoza, Vincent Regard, Pierre Antoine, Rodolfo Salas‐Gismondi, Rolando Bolaños,
Tópico(s)Geological formations and processes
ResumoResearch Article| June 01, 2007 How does the Nazca Ridge subduction influence the modern Amazonian foreland basin? N. Espurt; N. Espurt 1LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France, and IRD, Convenio IRD-PERUPETRO, Calle Teruel 357, Miraflores, Lima 18, Peru Search for other works by this author on: GSW Google Scholar P. Baby; P. Baby 1LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France, and IRD, Convenio IRD-PERUPETRO, Calle Teruel 357, Miraflores, Lima 18, Peru Search for other works by this author on: GSW Google Scholar S. Brusset; S. Brusset 2LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France Search for other works by this author on: GSW Google Scholar M. Roddaz; M. Roddaz 2LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France Search for other works by this author on: GSW Google Scholar W. Hermoza; W. Hermoza 3PERUPETRO, Convenio IRD-PERUPETRO, Avenida Luis Aldana 320, San Boja, Lima 41, Peru Search for other works by this author on: GSW Google Scholar V. Regard; V. Regard 4LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France Search for other works by this author on: GSW Google Scholar P.-O. Antoine; P.-O. Antoine 4LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France Search for other works by this author on: GSW Google Scholar R. Salas-Gismondi; R. Salas-Gismondi 5Museo de Historia Natural—UNMSM, Departamento de Paleontología de Vertebrados, Avenida Arenales 1256, Lima 14, Peru Search for other works by this author on: GSW Google Scholar R. Bolaños R. Bolaños 6PERUPETRO, Convenio IRD-PERUPETRO, Avenida Luis Aldana 320, San Boja, Lima 41, Peru Search for other works by this author on: GSW Google Scholar Author and Article Information N. Espurt 1LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France, and IRD, Convenio IRD-PERUPETRO, Calle Teruel 357, Miraflores, Lima 18, Peru P. Baby 1LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France, and IRD, Convenio IRD-PERUPETRO, Calle Teruel 357, Miraflores, Lima 18, Peru S. Brusset 2LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France M. Roddaz 2LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France W. Hermoza 3PERUPETRO, Convenio IRD-PERUPETRO, Avenida Luis Aldana 320, San Boja, Lima 41, Peru V. Regard 4LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France P.-O. Antoine 4LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Avenue Edouard Belin, F-31400 Toulouse, France R. Salas-Gismondi 5Museo de Historia Natural—UNMSM, Departamento de Paleontología de Vertebrados, Avenida Arenales 1256, Lima 14, Peru R. Bolaños 6PERUPETRO, Convenio IRD-PERUPETRO, Avenida Luis Aldana 320, San Boja, Lima 41, Peru Publisher: Geological Society of America Received: 26 Jul 2006 Revision Received: 26 Jan 2007 Accepted: 07 Feb 2007 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2007) 35 (6): 515–518. https://doi.org/10.1130/G23237A.1 Article history Received: 26 Jul 2006 Revision Received: 26 Jan 2007 Accepted: 07 Feb 2007 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 N. Espurt, P. Baby, S. Brusset, M. Roddaz, W. Hermoza, V. Regard, P.-O. Antoine, R. Salas-Gismondi, R. Bolaños; How does the Nazca Ridge subduction influence the modern Amazonian foreland basin?. Geology 2007;; 35 (6): 515–518. doi: https://doi.org/10.1130/G23237A.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 The subduction of an aseismic ridge has important consequences on the dynamics of the overriding upper plate. In the central Andes, the Nazca Ridge subduction imprint can be tracked on the eastern side of the Andes. The Fitzcarrald arch is the long-wavelength topography response of the Nazca Ridge flat subduction, 750 km inboard of the trench. This uplift is responsible for the atypical three-dimensional shape of the Amazonian foreland basin. The Fitzcarrald arch uplift is no older than Pliocene as constrained by the study of Neogene sediments and geomorphic markers, according to the kinematics of the Nazca Ridge subduction. 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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