Los domos graníticos de la Cuenca del Ridaura (Girona)

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dc.contributor.author Pallí i Buxó, Lluís
dc.date.issued 1996
dc.identifier.issn 0213-4497
dc.identifier.uri http://hdl.handle.net/10256/7192
dc.description.abstract Se describen los domos graníticos de la cuenca del río Ridaura. Sus caraterísticas geométricas se relacionan estrechamente con la disposición de las fracturas. Su génesis deriva de una fase subsuperficial, bajo un manto de alteración, presumiblemente desarrollada durante el Plioceno, y una fase de exhumación torrencial, que comprende desde el Plioceno terminal hasta la actualidad
dc.description.abstract This paper deals with the bornhardts of the Ridaura river area. Their geometrical characteristics are tightly related to the fracture system. These bornhardts evolve in two diferent stages: the first occurs under a regolith bed and develops during the Pliocene, and the later is an torrential stripping that extends from the latest Pliocene to the present
dc.format.mimetype application/pdf
dc.language.iso spa
dc.publisher Instituto Universitario de Geología "Isidro Parga Pondal"
dc.relation.isformatof Reproducció digital del document publicat a: http://www.iux.es/index.php?page=15&arts=57&id=3
dc.relation.ispartof © Cadernos do Laboratorio Xeoloxico de Laxe, 1996, núm. 21, p. 45-48
dc.relation.ispartofseries Articles publicats (D-CCAA)
dc.rights Tots els drets reservats
dc.subject Granit -- Afloraments -- Catalunya -- Ridaura (Curs d'aigua)
dc.subject Granite outcrops -- Catalonia -- Ridaura (River)
dc.title Los domos graníticos de la Cuenca del Ridaura (Girona)
dc.type info:eu-repo/semantics/article
dc.type.version info:eu-repo/semantics/publishedVersion

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