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• W2318371336 abstract "Research Article| January 01, 2013 Why has the Nazca plate slowed since the Neogene? Javier Quinteros; Javier Quinteros 1Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany2Department of Computer Sciences, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Buenos Aires C1428EGA, Argentina Search for other works by this author on: GSW Google Scholar Stephan V. Sobolev Stephan V. Sobolev 1Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany3Institute of Physics of the Earth, Russian Academy of Sciences, Moscow 123995, Russia Search for other works by this author on: GSW Google Scholar Author and Article Information Javier Quinteros 1Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany2Department of Computer Sciences, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Buenos Aires C1428EGA, Argentina Stephan V. Sobolev 1Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, 14473 Potsdam, Germany3Institute of Physics of the Earth, Russian Academy of Sciences, Moscow 123995, Russia Publisher: Geological Society of America Received: 08 Apr 2012 Revision Received: 11 Jun 2012 Accepted: 28 Jun 2012 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2012 Geological Society of America Geology (2013) 41 (1): 31–34. https://doi.org/10.1130/G33497.1 Article history Received: 08 Apr 2012 Revision Received: 11 Jun 2012 Accepted: 28 Jun 2012 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Javier Quinteros, Stephan V. Sobolev; Why has the Nazca plate slowed since the Neogene?. Geology 2013;; 41 (1): 31–34. doi: https://doi.org/10.1130/G33497.1 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 classic example of the not-well-understood rapid change of tectonic plate motion is the increase and then decrease of the convergence rate between the Nazca and South America plates during the past 25–20 m.y. that coincided with the growth of the Andes Mountains. Currently, the decrease in convergence rate is explained either by the increasing load of the Andes or by the appearance of flat slab segments beneath South America. Here, we present an alternative view based on a thermomechanical self-consistent (gravity driven) model of Nazca plate subduction. We explain the changes in the convergence rate as a natural consequence of the Nazca plate penetration into the transition zone and lower mantle after long-term oblique subduction of the Farallon plate. The model is consistent with seismic tomographic images of the Nazca plate beneath South America. Our model also shows that the presence of the Andes does not significantly affect the convergence rate between the Nazca and South America plates. 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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