Sedimentología de la formación Miers Bluff en los alrededores de la Base Antártica española. Isla Livingston. Shetland del Sur
The 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 fan La Formación...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | Spanish |
Published: |
Sociedad Geológica de España
1990
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Subjects: | |
Online Access: | http://hdl.handle.net/10272/18130 |
Summary: | The 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 fan La 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. |
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