Nota preliminar sobre la presencia de turmalinitas estratiformes en el Ordovícico Inferior de Latedo (NO de Zamora)

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dc.contributor.authorFernández Fernández, A.
dc.contributor.authorMoro Benito, M. C.
dc.date.accessioned2020-05-19T09:59:09Z
dc.date.available2020-05-19T09:59:09Z
dc.date.issued1991
dc.description.abstractIn this paper, the geological, texto-structural, mineralogical and chemical features of the stratiforme tourmalinites from the Lower Ordovician volcano-sedimentary Cabeza de las Viñas Formation (Alcañices Synforme), are given. According to these data, it is suggested that these tourmalinites has been originated by regional metamorphisme of the B-rich pelitic beds. The B were probably trought to the sediment by the hidrothermal solutions related with the underlayžng metabasaltic rocks existing in the studied areaes_ES
dc.identifier.urihttp://hdl.handle.net/10272/18005
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherStratiforme tourmaliniteses_ES
dc.subject.otherLower Ordovicianes_ES
dc.subject.otherRegional metamorphismees_ES
dc.subject.otherMetabasaltic rockses_ES
dc.titleNota preliminar sobre la presencia de turmalinitas estratiformes en el Ordovícico Inferior de Latedo (NO de Zamora)es_ES
dc.typejournal articlees_ES
dspace.entity.typePublication

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Geogaceta -- Nº 11, (1991)