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Sedimentology of the Myers Bluff Formation near the Spanish Antárctic Base, Livingston Island, South Shetlands

dc.contributor.authorArche, A.
dc.contributor.authorLópez Martínez, Jerónimo
dc.contributor.authorMartínez de Pisón, E.
dc.date.accessioned2020-06-03T08:38:37Z
dc.date.available2020-06-03T08:38:37Z
dc.date.issued1990
dc.identifier.urihttp://hdl.handle.net/10272/18130
dc.description.abstractThe Miers Bluff Formation crops out in the Hurd Peninsula, Livingston Island. lt consist of greywackes and slates, organised in coarsening-thickening and fining-thinning cycles. They have been interpreted as channellised and non-channellised turbidites from a mid- and outer turbiditic fanes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAn error occurred on the license name.*
dc.rights.uriAn error occurred getting the license - uri.*
dc.subject.otherSedimentologyes_ES
dc.subject.otherTurbiditeses_ES
dc.subject.otherMiers Bluff Formationes_ES
dc.subject.otherLivingston Islandes_ES
dc.subject.otherSouth Shetlandes_ES
dc.subject.otherAntarcticaes_ES
dc.titleSedimentología de la formación Miers Bluff en los alrededores de la Base Antártica española. Isla Livingston. Shetland del Sures_ES
dc.titleSedimentology of the Myers Bluff Formation near the Spanish Antárctic Base, Livingston Island, South Shetlandseng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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