DUGiDocsMajor-elements trends in cenozoic volcanites of Hungary
dc.contributor.author
dc.contributor.editor
dc.date.accessioned
2008-05-05T14:36:18Z
dc.date.available
2008-05-05T14:36:18Z
dc.date.issued
2003-10-16
dc.identifier.citation
Martín Fernández, J.A.; Barceló i Vidal, C.; Pawlowsky Glahn, V.; Kovács, L.Ó.; Kovács, G.P. 'Major-elements trends in cenozoic volcanites of Hungary' a CODAWORK’03. Girona: La Universitat, 2003 [consulta: maig 2008]. Necessita Adobe Acrobat. Disponible a Internet a: http://hdl.handle.net/10256/679
dc.identifier.isbn
84-8458-111-X
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dc.description.abstract
Hungary lies entirely within the Carpatho-Pannonian Region (CPR), a dominant tectonic unit of eastern Central Europe. The CPR consists of the Pannonian Basin system, and the arc of the Carpathian Mountains surrounding the lowlands in the north, east, and southeast. In the west, the CPR is bounded by the Eastern Alps, whereas in the south, by the Dinaridic belt. (...)
dc.description.sponsorship
Geologische Vereinigung; Universitat de Barcelona, Equip de Recerca Arqueomètrica; Institut d’Estadística de Catalunya; International Association for Mathematical Geology; Patronat de l’Escola Politècnica Superior de la Universitat de Girona; Fundació privada: Girona, Universitat i Futur.
dc.format.mimetype
application/pdf
dc.language.iso
eng
dc.publisher
Universitat de Girona. Departament d’Informàtica i Matemàtica Aplicada
dc.rights
Tots els drets reservats
dc.title
Major-elements trends in cenozoic volcanites of Hungary
dc.type
info:eu-repo/semantics/conferenceObject
dc.rights.accessRights
info:eu-repo/semantics/openAccess