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<identifier>oai:HAL:hal-00407200v1</identifier>
<datestamp>2018-01-11</datestamp>
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<setSpec>subject:sdu</setSpec>
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<metadata><dc>
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<title lang=en>Predicting trench and plate motion from the dynamics of a strong slab</title>
<creator>Faccenna, C.</creator>
<creator>Heuret, Arnauld</creator>
<creator>Funiciello, F.</creator>
<creator>Lallemand, Serge</creator>
<creator>Becker, T. W.</creator>
<contributor>Dipartimento Scienze Geologiche, Università Roma TRE, Roma ; Université du Québec</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>Department of Earth Sciences, University of Southern California, Los Angeles ; Université du Québec</contributor>
<source>ISSN: 0012-821X</source>
<source>Earth and Planetary Science Letters</source>
<publisher>Elsevier</publisher>
<identifier>hal-00407200</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00407200</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00407200</source>
<source>Earth and Planetary Science Letters, Elsevier, 2007, 257 (1-2), pp.29-36. 〈10.1016/j.epsl.2007.02.016〉</source>
<identifier>DOI : 10.1016/j.epsl.2007.02.016</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.epsl.2007.02.016</relation>
<language>en</language>
<subject lang=en>subduction</subject>
<subject lang=en>oceanic plate</subject>
<subject lang=en>trench</subject>
<subject lang=en>laboratory experiments</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The motion of oceanic plates is commonly related to the subduction of cold and dense oceanic material into the mantle. These models predict plate velocities from subduction velocities but the trench motion is not directly included in the computation. Here, using a recent compilation of a global data set, we found that the motion of trenches (either advancing or retreating with respect to upper plates) scales with their corresponding subducting plates motion. Based on simple experimental tests, we found that subduction of strong slabs inside the upper mantle correctly predicts these kinematic relationships. We deduce that the motion of the trenches represent the surface manifestation of the resistance encountered by the subducting lithosphere to bend and penetrate within the upper mantle.</description>
<date>2007</date>
</dc>
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