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dc.contributor.authorRiguzzi, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italia-
dc.contributor.authorPanza, G.; Dipartimento di Scienze della Terra, Università di Trieste, and ICTP, Italy-
dc.contributor.authorVarga, P.; Geodetic and Geophysical Research Institute, Seismological Observatory, Budapest, Hungary-
dc.contributor.authorDoglioni, C.; Dipartimento di Scienze della Terra, Università Sapienza, Roma, Italy-
dc.date.accessioned2010-05-18T12:19:59Z-
dc.date.available2010-05-18T12:19:59Z-
dc.date.issued2010-03-19-
dc.identifier.urihttp://hdl.handle.net/2122/6011-
dc.description.abstractWe re-evaluate the possibility that Earth's rotation contributes to plate tectonics on the basis of the following observations: 1) plates move along a westerly polarized flow that forms an angle relative to the equator close to the revolution plane of the Moon; 2) plate boundaries are asymmetric, being their geographic polarity the first order controlling parameter; unlike recent analysis, the slab dip is confirmed to be steeper along W-directed subduction zones; 3) the global seismicity depends on latitude and correlates with the decadal oscillations of the excess length of day (LOD); 4) the Earth's deceleration supplies energy to plate tectonics comparable to the computed budget dissipated by the deformation processes; 5) the Gutenberg–Richter law supports that the whole lithosphere is a self-organized system in critical state, i.e., a force is acting contemporaneously on all the plates and distributes the energy over the whole lithospheric shell, a condition that can be satisfied by a force acting at the astronomical scale. Assuming an ultra-low viscosity layer in the upper asthenosphere, the horizontal component of the tidal oscillation and torque would be able to slowly shift the lithosphere relative to the mantle.en_US
dc.description.sponsorshipHungarian Scientific Research Fund OTKA in the framework of project K 60394en_US
dc.language.isoengen_US
dc.publisher.nameElsevieren_US
dc.relation.ispartofTectonophysicsen_US
dc.relation.ispartofseries1-4/484 (2010)en_US
dc.subjectPlate tectonicsen_US
dc.subjectEarth's rotationen_US
dc.subjectTidal despinningen_US
dc.subjectEarth's energy budgeten_US
dc.titleCan Earth's rotation and tidal despinning drive plate tectonics?en_US
dc.typearticle-
dc.description.statusPublisheden_US
dc.type.QualityControlPeer-revieweden_US
dc.description.pagenumber60-73en_US
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamicsen_US
dc.identifier.doi10.1016/j.tecto.2009.06.012en_US
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dc.description.obiettivoSpecifico3.3. Geodinamica e struttura dell'interno della Terraen_US
dc.description.journalTypeJCR Journalen_US
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04.07.02. Geodynamics

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