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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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 |
_version_ |
1790601902752268288 |