Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7928
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dc.contributor.authorallScalera, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.date.accessioned2012-04-02T07:20:08Zen
dc.date.available2012-04-02T07:20:08Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/7928en
dc.descriptionIn this paper the theory of the plate tectonics is interpreted as a Tychonic conception. The expanding Earth is the more complete description of the geologic reality.en
dc.description.abstractThe Danish astronomer Tycho Brahe (1546–1601) developed a model of the universe – the Tychonic system – by combining the Ptolemaic system with the Copernican system. In the Tychonic (geocentric) system the Moon and the Sun were considered to revolve around the Earth, while the planets (Mercury, Venus, Mars, Jupiter and Saturn) revolve around the Sun. In this paper the theory of the plate tectonics is interpreted as a Tychonic conception because – making several compromises – fixism and mobilism are mixed in a unique pattern, in which the compression and the extension are unified in a compressional interpretation (see the coexistence of trenches and orogenic chains on the active continental margins), while, conversely, the fold-belts and the mid-oceanic ridges are separated into two different geodynamic domains. For all these cases, the extensional description could be more appropriate.en
dc.description.sponsorshipINGV - Roma1en
dc.language.isoEnglishen
dc.publisher.nameVerlag für Geowissenschaften, Berlinen
dc.relation.ispartofZeitschrift für geologische Wissenschaftenen
dc.relation.ispartofseries/40 (2012)en
dc.subjectExpanding Earthen
dc.subjectPlate tectonicsen
dc.subjectGlobal geodynamicsen
dc.subjectParadoxes in Earth Sciencesen
dc.titleIs plate tectonics a Tychonian compromise?en
dc.title.alternativeIst die Plattentektonik ein Tychonischer Kompromiß?en
dc.title.alternativeLa tettonica a placche è un compromesso Ticonico?en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber19-34en
dc.identifier.URLhttp://www.zgw-online.de/en/en
dc.identifier.URLhttp://www.zgw-online.de/en/pages/_volume2012.phpen
dc.subject.INGV04. Solid Earth::04.01. Earth Interior::04.01.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.01. Earth Interior::04.01.02. Geological and geophysical evidences of deep processesen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneousen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamicsen
dc.description.obiettivoSpecifico3.3. Geodinamica e struttura dell'interno della Terraen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextrestricteden
dc.contributor.authorScalera, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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