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dc.contributor.authorPagés Valcarlos, J. L.
dc.date.accessioned2010-01-25T09:33:46Z
dc.date.available2010-01-25T09:33:46Z
dc.date.issued1998
dc.identifier.citationCadernos do Laboratorio Xeolóxico de Laxe, 1998, 23: 27-41 ISSN: 00213-4497es_ES
dc.identifier.issn0213-4497
dc.identifier.urihttp://hdl.handle.net/2183/6377
dc.description.abstract[Abstract] This paper deals with the analysis of the geology and structure of the pegmoaplitic field of Doade (Ourense, Spain). Several bodies are distinguished taking into account their mineralogy and spatial distribution. The composition shows the existence of four types of pegmoaplites, all of them corresponding to the same family in different evolutionary stages, in accordance with their spatial distribution (a clear zonality from the granite boundary into the metamorphic rock). Also the study of the greinesization process and the casiterite contain is carried out.
dc.language.isospaes_ES
dc.publisherUniversidade da Coruñaes_ES
dc.subjectPegmoaplitees_ES
dc.subjectZonalityes_ES
dc.subjectCassiteriteses_ES
dc.subjectGreisenizationes_ES
dc.subjectOurensees_ES
dc.titleEl campo pegmoaplítico de Doade (Ourense) y sus mineralizaciones de Sn y Ta asociadases_ES
dc.title.alternativeThe pegmoaplitic field of Doade (Ourense, Spain) and associated Sn and Ta mineralizations
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccess


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