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Structural features of the sedimentary rocks of Macaronesia

dc.contributor.authorMitchell-Thomé, R. C.
dc.date.accessioned2017-12-13T18:55:26Z
dc.date.available2017-12-13T18:55:26Z
dc.date.issued1981-07
dc.description.abstractThe sediments within the five Maraconesian archipelagos of the Azores, Madeira, Selvagens, Canaries and Cape Verde are referred to. Lithology, structural features, outcrop areas, thicknesses, maximum dips, inland extents, highest elevations and stratigraphic ages are remarked upon. The very uneven distribution of sedimentaries within the various archipelagos is noted, and a possible cause for the great thickness and older age of such in the Canaries and Cape Verde, as also their scarcity in the Azores, is given.en
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationMITCHELL-THOMÉ, R. C. (1981). Structural features of the sedimentary rocks of Macaronesia. "Arquipélago. Série Ciências da Natureza", 2: 121-151.pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.3/4508
dc.language.isoengpt_PT
dc.publisherUniversidade dos Açorespt_PT
dc.subjectSedimentary Rocksen
dc.subjectMacaronesiapt_PT
dc.titleStructural features of the sedimentary rocks of Macaronesiaen
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePonta Delgada, Açorespt_PT
oaire.citation.endPage151pt_PT
oaire.citation.startPage121pt_PT
oaire.citation.titleArquipélago. Série Ciências da Naturezapt_PT
oaire.citation.volume2pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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