Arche, A.López Martínez, JerónimoMartínez de Pisón, E.2020-06-032020-06-031990http://hdl.handle.net/10272/18130The 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 channelised and non-channelised turbidites from a mid- and outer turbiditic fanLa Formación Miers Bluff aflora en la península de Hurd, Isla de Livingston. Está compuesta por grauvacas y pizarra, organizadas en ciclos de engrosamiento-espesamiento y estabilizante-adelgazamiento. Se han interpretado como turbiditas canalizadas y no canalizadas de un abanico turbidítico medio y exterior.spaAn error occurred on the license name.An error occurred getting the license - uri.SedimentologyTurbiditesMiers Bluff FormationLivingston IslandSouth ShetlandAntarcticaSedimentología de la formación Miers Bluff en los alrededores de la Base Antártica española. Isla Livingston. Shetland del SurSedimentology of the Myers Bluff Formation near the Spanish Antárctic Base, Livingston Island, South Shetlandsjournal articleopen access