Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/1140
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dc.contributor.authorallScalera, G.; Istituto Nazionale di Geofisica Roma, Italyen
dc.date.accessioned2006-04-24T12:31:14Zen
dc.date.available2006-04-24T12:31:14Zen
dc.date.issued1993-09en
dc.identifier.urihttp://hdl.handle.net/2122/1140en
dc.description.abstractIt is shown how shape between certain ocean basins and continents create serious difficulties to the concept of subduction and can be considered evidence of a non-chaotic emplacement of the arc-trench zones along pre-existing deep geofractures, which are related to shapes of far continents. These similarities point to a fundamental process which cannot be described by the plate tectonics and other tectonic hypotheses, and which is till now mostly hidden to our understanding. Because the similarities are also clues of a former proximity of the circumpacific continents, an expanding earth appears favoured by this new observational evidence.en
dc.format.extent1909953 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.relation.ispartofseries5-6/36 (1993)en
dc.subjectglobal tectonicsen
dc.subjectgeomorphologyen
dc.titleNon-chaotic emplacements of trench-arc zones in the Pacific Hemisphereen
dc.typearticleen
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonicsen
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorScalera, G.en
dc.contributor.departmentIstituto 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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