Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1496
DC FieldValueLanguage
dc.contributor.authorallScalera, G.; stituto Nazionale di Geofisica, Roma, Italyen
dc.date.accessioned2006-08-02T13:18:43Zen
dc.date.available2006-08-02T13:18:43Zen
dc.date.issued1998-11en
dc.identifier.urihttp://hdl.handle.net/2122/1496en
dc.description.abstractThe present research concerns the study of the possibility of an increase in the size of the Earthbecause of a still unknown process. After a previous recognition of the existence in the Pacific of shape conformities in a number of pairs of continental and oceanic boundaries (Scalera, 1991, 1993a), a search for compatibility of these results with independent data sets, paleomagnetic and geological and paleontological was undertaken. The conclusion is that the Earth's dilatation is compatible with the used data, while nothing can be affirmed with certainty about the dilatation process or its continuity or discontinuity through geological time. A tentative model of the evolution of the trench-arc-backarc systems has been provided, tuning it in agreement with a dilatational planet.en
dc.format.extent2361219 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries5-6/41 (1998)en
dc.subjectpaleogeographyen
dc.subjectglobal tectonicsen
dc.subjectEarth expansionen
dc.titlePaleogeographical reconstructions compatible with Earth dilatationen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamicsen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorScalera, G.en
dc.contributor.departmentstituto Nazionale di Geofisica, Roma, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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