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

15 pages, 9 figures, 1 table 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-m...

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Published in:Geological Society, London, Special Publications
Main Authors: Casas, David, García, Marga, Bohoyo, Fernando, Maldonado, Andrés, Ercilla, Gemma
Format: Book Part
Language:unknown
Published: Geological Society of London 2018
Subjects:
Online Access:http://hdl.handle.net/10261/163635
https://doi.org/10.1144/SP461.10
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spelling ftcsic:oai:digital.csic.es:10261/163635 2024-02-11T09:57:51+01:00 The Gebra-Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica) Casas, David García, Marga Bohoyo, Fernando Maldonado, Andrés Ercilla, Gemma 2018 http://hdl.handle.net/10261/163635 https://doi.org/10.1144/SP461.10 unknown Geological Society of London #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2015-65461-C2-2-R https://doi.org/10.1144/SP461.10 Sí issn: 0305-8719 e-issn: 2041-4927 Exploration of Subsurface Antarctica: Uncovering Past Changes and Modern Processes: 61-75 (2018) Geological Society Special Publication 461: 61-75 (2018) 978-1-78620-322-9 http://hdl.handle.net/10261/163635 doi:10.1144/SP461.10 none capítulo de libro http://purl.org/coar/resource_type/c_3248 2018 ftcsic https://doi.org/10.1144/SP461.10 2024-01-16T10:29:52Z 15 pages, 9 figures, 1 table 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 This study was supported by the Spanish projects MAGIA (ANT97-0584), CONPACA (CTM2011-30241-C02/01ANT), TASMANDRAKE (CTM2014-60451-C2-02/01), MOWER (CTM2012-39599-C03) and FAUCES (CTM2015-65461-C2-1-R) Peer Reviewed Book Part Antarc* Antarctic Antarctic Peninsula Antarctica 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 unknown
description 15 pages, 9 figures, 1 table 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 This study was supported by the Spanish projects MAGIA (ANT97-0584), CONPACA (CTM2011-30241-C02/01ANT), TASMANDRAKE (CTM2014-60451-C2-02/01), MOWER (CTM2012-39599-C03) and FAUCES (CTM2015-65461-C2-1-R) Peer Reviewed
format Book Part
author Casas, David
García, Marga
Bohoyo, Fernando
Maldonado, Andrés
Ercilla, Gemma
spellingShingle Casas, David
García, Marga
Bohoyo, Fernando
Maldonado, Andrés
Ercilla, Gemma
The Gebra-Magia Complex: mass-transport processes reworking trough-mouth fans in the Central Bransfield Basin (Antarctica)
author_facet Casas, David
García, Marga
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 2018
url http://hdl.handle.net/10261/163635
https://doi.org/10.1144/SP461.10
geographic Antarctic
Antarctic Peninsula
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
op_relation #PLACEHOLDER_PARENT_METADATA_VALUE#
info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2015-65461-C2-2-R
https://doi.org/10.1144/SP461.10

issn: 0305-8719
e-issn: 2041-4927
Exploration of Subsurface Antarctica: Uncovering Past Changes and Modern Processes: 61-75 (2018)
Geological Society Special Publication 461: 61-75 (2018)
978-1-78620-322-9
http://hdl.handle.net/10261/163635
doi:10.1144/SP461.10
op_rights none
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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