Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/6011| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Riguzzi, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italia | en |
| dc.contributor.authorall | Panza, G.; Dipartimento di Scienze della Terra, Università di Trieste, and ICTP, Italy | en |
| dc.contributor.authorall | Varga, P.; Geodetic and Geophysical Research Institute, Seismological Observatory, Budapest, Hungary | en |
| dc.contributor.authorall | Doglioni, C.; Dipartimento di Scienze della Terra, Università Sapienza, Roma, Italy | en |
| dc.date.accessioned | 2010-05-18T12:19:59Z | en |
| dc.date.available | 2010-05-18T12:19:59Z | en |
| dc.date.issued | 2010-03-19 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/6011 | en |
| dc.description.abstract | We 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 |
| dc.description.sponsorship | Hungarian Scientific Research Fund OTKA in the framework of project K 60394 | en |
| dc.language.iso | English | en |
| dc.publisher.name | Elsevier | en |
| dc.relation.ispartof | Tectonophysics | en |
| dc.relation.ispartofseries | 1-4/484 (2010) | en |
| dc.subject | Plate tectonics | en |
| dc.subject | Earth's rotation | en |
| dc.subject | Tidal despinning | en |
| dc.subject | Earth's energy budget | en |
| dc.title | Can Earth's rotation and tidal despinning drive plate tectonics? | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | 60-73 | en |
| dc.subject.INGV | 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics | en |
| dc.identifier.doi | 10.1016/j.tecto.2009.06.012 | en |
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| dc.description.obiettivoSpecifico | 3.3. Geodinamica e struttura dell'interno della Terra | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | reserved | en |
| dc.contributor.author | Riguzzi, F. | en |
| dc.contributor.author | Panza, G. | en |
| dc.contributor.author | Varga, P. | en |
| dc.contributor.author | Doglioni, C. | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en |
| dc.contributor.department | Dipartimento di Scienze della Terra, Università di Trieste, and ICTP, Italy | en |
| dc.contributor.department | Geodetic and Geophysical Research Institute, Seismological Observatory, Budapest, Hungary | en |
| dc.contributor.department | Dipartimento di Scienze della Terra, Università Sapienza, Roma, Italy | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
| crisitem.author.dept | Geodetic and Geophysical Research Institute, Seismological Observatory, Budapest, Hungary | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione AC, Roma, Italia | - |
| crisitem.author.orcid | 0000-0003-3453-5110 | - |
| crisitem.author.orcid | 0000-0002-8651-6387 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
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