Sedimentología de la formación Miers Bluff en los alrededores de la Base Antártica española. Isla Livingston. Shetland del Sur
The Míers Bluff Formation crops out ín the Hurd Península, Livíngston Island. It consíst of greywackes and slates, organísed ín coarseníng-thíckeníng and fíníng-thínníng cycles. They have been ínterpreted as channellísed and non-channellísed turbídites from a míd- and outer turbídítíc fan....
| Autores: | , , |
|---|---|
| Tipo de documento: | artigo |
| Data de publicação: | 1991 |
| País: | España |
| Recursos: | Universidad Complutense de Madrid (UCM) |
| Repositório: | Docta Complutense |
| Idioma: | espanhol |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/57833 |
| Acesso em linha: | https://hdl.handle.net/20.500.14352/57833 |
| Access Level: | Acceso aberto |
| Palavra-chave: | 551.3.051(99) Sedímentology Turbídítes Míers Bluff Formatíon Livíngston Island South Shetland Antarctíca Geología estratigráfica 2506.19 Estratigrafía |
| Resumo: | The Míers Bluff Formation crops out ín the Hurd Península, Livíngston Island. It consíst of greywackes and slates, organísed ín coarseníng-thíckeníng and fíníng-thínníng cycles. They have been ínterpreted as channellísed and non-channellísed turbídites from a míd- and outer turbídítíc fan. |
|---|