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dc.contributor.authorVidal Romaní, Juan Ramón
dc.contributor.authorRamanohison, H.
dc.contributor.authorRabenandrasana, S.
dc.date.accessioned2010-01-22T13:26:36Z
dc.date.available2010-01-22T13:26:36Z
dc.date.issued1997
dc.identifier.citationCadernos do Laboratorio Xeolóxico de Laxe, 1997, 22: 183-208 ISSN: 0213-4497es_ES
dc.identifier.issn0213-4497
dc.identifier.urihttp://hdl.handle.net/2183/6287
dc.description.abstract[Abstract] The Andringirra Massif is a srratoide granite on the south of the Isle of Madagascar. Is a residual reliefwhich represents one ofthe last remnants of the Gondwana surface at the island egraded after the break of the supercontinent.Three different levels at 2500m, 2000m and 1500m of altitude with the etche forms associated show different stages at the evolution of the massif. Over these pediments was preserved different kinds of granite etche forms at different stages ofevolution with a very clear relation with the surface age younger fram the top to the bottom of the massif. After the exposure of the etched relief, the corresponding forms evolves suabaerially which signify that they shows two stages of evolution: one subedaphical the other subaerial.
dc.language.isofraes_ES
dc.publisherUniversidade da Coruñaes_ES
dc.subjectGranite geomorphologyes_ES
dc.subjectAndringitraes_ES
dc.subjectMassifes_ES
dc.subjectCenozoices_ES
dc.subjectMadagascares_ES
dc.titleGéomorphologue granitique du Massif de l'Andringitra: Sa relation avec l'évolution de l'Île pendant le Cénozoïquees_ES
dc.title.alternativeGranite geomorphology of Andringirra Massif and their relation with the cenozoic evolurion of rhe Isle
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccess


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