The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica)

The Gebra–Magia Complex is an important example of a submarine mass-movement composite located on the lower continental slope of the Antarctic Peninsula (Central Bransfield Basin). Continuous instability dynamics over time is inferred to have affected the palaeo-trough-mouth fans present in the stud...

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Published in:Geological Society, London, Special Publications
Main Authors: Casas, David, García, M., Bohoyo, Fernando, Maldonado, Andrés, Ercilla, Gemma
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of London 2017
Subjects:
Online Access:http://hdl.handle.net/10261/277185
https://doi.org/10.1144/SP461.10
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record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/277185 2024-02-11T09:56:16+01:00 The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica) Casas, David García, M. Bohoyo, Fernando Maldonado, Andrés Ercilla, Gemma Cuenca central de Bransfield, Antártida 2017-06-16 http://hdl.handle.net/10261/277185 https://doi.org/10.1144/SP461.10 en eng Geological Society of London https://sp.lyellcollection.org/content/461/1/61 Geological Society Special Publications, vol.461, 61-75 2041-4927 http://hdl.handle.net/10261/277185 https://doi.org/10.1144/SP461.10 open fondo marino movimiento masa Sedimentación Geomorfología Tectónica Antártida artículo 2017 ftcsic https://doi.org/10.1144/SP461.10 2024-01-16T11:27:54Z The Gebra–Magia Complex is an important example of a submarine mass-movement composite located on the lower continental slope of the Antarctic Peninsula (Central Bransfield Basin). Continuous instability dynamics over time is inferred to have affected the palaeo-trough-mouth fans present in the study area. The depositional architecture and the outstanding relief of the Gebra Valley, which is the most striking morphological feature in the area, determine the asymmetrical morphology of the complex. This complex is characterized, from east to west, by an open-slope margin flanking the sidewall of the Gebra Valley, the Gebra Valley itself and a SW margin that is connected to the Magia area by a large scar approximately 7.8 km to the SW. The Gebra Valley is a Quaternary debris valley resulting from repeated large-scale mass-transport and cut-and-fill processes. In contrast, the Magia area is dominated by unchannelized sedimentary instability processes, resulting in a different sedimentary architecture and morphology. The near-surface sediments in the Gebra–Magia Complex document the continuous occurrence of recent mass movements, as also evidenced by flows transported downslope as unchannelized or channelized flows. Climate and tectonic activity are considered the primary factors controlling the development of the complex. Instituto Geológico y Minero de España, España Instituto Andaluz de Ciencias de la Tierra, España Institut de Ciències del Mar, Consejo Superior de Investigaciones Científicas, España Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Antártida Digital.CSIC (Spanish National Research Council) Antarctic Antarctic Peninsula The Antarctic Geological Society, London, Special Publications 461 1 61 75
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic fondo marino
movimiento masa
Sedimentación
Geomorfología
Tectónica
Antártida
spellingShingle fondo marino
movimiento masa
Sedimentación
Geomorfología
Tectónica
Antártida
Casas, David
García, M.
Bohoyo, Fernando
Maldonado, Andrés
Ercilla, Gemma
The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica)
topic_facet fondo marino
movimiento masa
Sedimentación
Geomorfología
Tectónica
Antártida
description The Gebra–Magia Complex is an important example of a submarine mass-movement composite located on the lower continental slope of the Antarctic Peninsula (Central Bransfield Basin). Continuous instability dynamics over time is inferred to have affected the palaeo-trough-mouth fans present in the study area. The depositional architecture and the outstanding relief of the Gebra Valley, which is the most striking morphological feature in the area, determine the asymmetrical morphology of the complex. This complex is characterized, from east to west, by an open-slope margin flanking the sidewall of the Gebra Valley, the Gebra Valley itself and a SW margin that is connected to the Magia area by a large scar approximately 7.8 km to the SW. The Gebra Valley is a Quaternary debris valley resulting from repeated large-scale mass-transport and cut-and-fill processes. In contrast, the Magia area is dominated by unchannelized sedimentary instability processes, resulting in a different sedimentary architecture and morphology. The near-surface sediments in the Gebra–Magia Complex document the continuous occurrence of recent mass movements, as also evidenced by flows transported downslope as unchannelized or channelized flows. Climate and tectonic activity are considered the primary factors controlling the development of the complex. Instituto Geológico y Minero de España, España Instituto Andaluz de Ciencias de la Tierra, España Institut de Ciències del Mar, Consejo Superior de Investigaciones Científicas, España
format Article in Journal/Newspaper
author Casas, David
García, M.
Bohoyo, Fernando
Maldonado, Andrés
Ercilla, Gemma
author_facet Casas, David
García, M.
Bohoyo, Fernando
Maldonado, Andrés
Ercilla, Gemma
author_sort Casas, David
title The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica)
title_short The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica)
title_full The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica)
title_fullStr The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica)
title_full_unstemmed The Gebra–Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica)
title_sort gebra–magia complex: mass-transport processes reworking trough-mouth fans in the central bransfield basin (antarctica)
publisher Geological Society of London
publishDate 2017
url http://hdl.handle.net/10261/277185
https://doi.org/10.1144/SP461.10
op_coverage Cuenca central de Bransfield, Antártida
geographic Antarctic
Antarctic Peninsula
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Antártida
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Antártida
op_relation https://sp.lyellcollection.org/content/461/1/61
Geological Society Special Publications, vol.461, 61-75
2041-4927
http://hdl.handle.net/10261/277185
https://doi.org/10.1144/SP461.10
op_rights open
op_doi https://doi.org/10.1144/SP461.10
container_title Geological Society, London, Special Publications
container_volume 461
container_issue 1
container_start_page 61
op_container_end_page 75
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