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<identifier>oai:HAL:hal-00682150v1</identifier>
<datestamp>2018-01-11</datestamp>
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<title lang=en>On the role of slab pull in the Cenozoic motion of the Pacific plate</title>
<creator>Faccenna, Claudio</creator>
<creator>Becker, Thorsten W.</creator>
<creator>Lallemand, Serge</creator>
<creator>Steinberger, Bernhard</creator>
<contributor>Università degli Studi Roma Tre</contributor>
<contributor>University of Southern California (USC)</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>GeoForschungsZentrum - Helmholtz-Zentrum Potsdam (GFZ)</contributor>
<description>International audience</description>
<source>ISSN: 0094-8276</source>
<source>EISSN: 1944-8007</source>
<source>Geophysical Research Letters</source>
<publisher>American Geophysical Union</publisher>
<identifier>hal-00682150</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00682150</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00682150/document</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00682150/file/faccennaGRL2012.pdf</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00682150</source>
<source>Geophysical Research Letters, American Geophysical Union, 2012, 39, pp.L03305. 〈10.1029/2011GL050155〉</source>
<identifier>DOI : 10.1029/2011GL050155</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2011GL050155</relation>
<language>en</language>
<subject lang=es>Pacific</subject>
<subject lang=es>subduction</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>We analyze the role of slab pull acting on the Pacific plate during its early Tertiary change in motion. Slab pull forces are estimated by integrating the negative buoyancy of a 700 km long slab along a revised subduction boundary model adopting the Muller et al. (2008) seafloor age reconstructions. Our results indicate that torques predicted from a simple slab pull model match the Pacific plate Euler vectors during the Tertiary fairly well. The change of the Pacific motion at similar to 50-40 Ma appears to be driven by the onset of the Izu-Bonin-Mariana system and, soon afterwards, by the Tonga-Kermadec subduction zones.</description>
<date>2012</date>
</dc>
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