Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5124
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dc.contributor.authorallbozic, zeljko; noneen
dc.date.accessioned2009-07-19T22:15:19Zen
dc.date.available2009-07-19T22:15:19Zen
dc.date.issued2009-07en
dc.identifier.urihttp://hdl.handle.net/2122/5124en
dc.description.abstractNowdays we can easily take for a fact the existance of ancient supercontinent named Pangea.If one just takes a glance at borderlines of modern continents one can conclude,without further argument,that they were once conjoined indeed.But the process of development and the process of disintegration of Pangea still inflames bitter arguments. New concept in global tectonics endorses two-layered lithosphere: Primary Layer: One that covers all of the Earths surface,and Secondary Layer: One that exists on top of Primery layer and consists of Earths continents (originated as Pangea). Therefor,covering aproximetly one quarter of Earths surface.en
dc.description.sponsorshipnoneen
dc.language.isoEnglishen
dc.subjecttectonicsen
dc.subjectlithosphereen
dc.titlenew concept in global tectonicsen
dc.title.alternativenoen
dc.typethesisen
dc.description.statusUnpublisheden
dc.identifier.URLn/aen
dc.subject.INGV04. Solid Earth::04.07. Tectonophysics::04.07.04. Plate boundaries, motion, and tectonicsen
dc.type.methodconcepten
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.fulltextopenen
dc.contributor.authorbozic, zeljkoen
dc.contributor.departmentnoneen
item.openairetypethesis-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_46ec-
item.fulltextWith Fulltext-
crisitem.classification.parent04. Solid Earth-
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