Erosive sub-circular depressions on the Guadalquivir Bank (Gulf of Cadiz): Interaction between bottom current, mass-wasting and tectonic processes

Special issue The contourite log-book: significance for palaeoceanography, ecosystems and slope instability.-- 15 pages, 9 figures

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Main Authors: García, Marga, Hernández-Molina, Francisco J., Alonso, Belén, Vázquez, Juan Tomás, Ercilla, Gemma, Llave, Estefanía, Casas, David
Other Authors: Ministerio de Economía y Competitividad (España)
Format: artículo biblioteca
Published: Elsevier 2016-08
Subjects:Gulf of Cadiz, Contourite depositional systems, Erosional features, Morphology, Seismic stratigraphy, Mediterranean Outflow Water,
Online Access:http://hdl.handle.net/10261/135510
http://dx.doi.org/10.13039/501100003329
http://dx.doi.org/10.13039/501100011011
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spelling dig-icm-es-10261-1355102019-10-03T07:35:01Z Erosive sub-circular depressions on the Guadalquivir Bank (Gulf of Cadiz): Interaction between bottom current, mass-wasting and tectonic processes García, Marga Hernández-Molina, Francisco J. Alonso, Belén Vázquez, Juan Tomás Ercilla, Gemma Llave, Estefanía Casas, David Ministerio de Economía y Competitividad (España) Junta de Andalucía Gulf of Cadiz Contourite depositional systems Erosional features Morphology Seismic stratigraphy Mediterranean Outflow Water Special issue The contourite log-book: significance for palaeoceanography, ecosystems and slope instability.-- 15 pages, 9 figures Morphological features (escarpments, depressions and valleys) identified on the Guadalquivir Bank, within the middle slope of the Gulf of Cadiz, have been investigated based on high- and mid-resolution geophysical datasets. The morphological and seismic stratigraphic analyses allowed their interpretation as the result of the interaction between oceanographic, mass-wasting and tectonic processes. A phase of enhanced tectonic activity occurred during the Mid-Pleistocene related to the activity of diapiric structures, the front of the allochthonous units, and/or basement uplift or adjustments. This event seems crucial for the origin of widespread mass-wasting events along middle slope sheeted drift plateaus that have been further reworked by the Mediterranean Outflow Water. This resulted in the erosion of a marginal valley to the north of the Guadalquivir Bank, while fluid escape processes also have a minor role in the creation of crescent-shaped depressions. The Diego Cao channel is the result of a complex evolution, from a contourite moat associated to a separated drift to a multi-crested drift and moat system during the Pliocene and Early Quaternary. During the Mid-Pleistocene, the mass-wasting phase produced a prominent erosive surface that opened a deep gateway into the Guadalquivir Bank uplifted basement, allowing the onset of the Mediterranean Intermediate Branch to flow towards the N-NW. The system evolved into a contourite system composed of the present-day channel and an associated deposit on its western side (Bartolomeu Dias sheeted drift plateau) that forms a particularly complex separated drift. This drift displays a series of circular depressions that are similar in morphology to collapse features or pockmarks, but are in contrast, the result of the interaction between the bottom current and the irregular mass-wasting-related scars This research is part of the projects MONTERA (CTM-14157-C02-02) and MOWER (CTM-2012-395599-C03) funded by the Spanish Ministry of Economy and Competitiveness. The research of Marga Garcia has been funded by a Juan de la Cierva Grant (Spanish Ministry of Economy and Competitiveness) and a Talentia Grant (Junta de Andalucia and European Union, grant reference 267226) Peer Reviewed 2016-08-12T06:31:15Z 2016-08-12T06:31:15Z 2016-08 2016-08-12T06:31:16Z artículo http://purl.org/coar/resource_type/c_6501 doi: 10.1016/j.margeo.2015.10.004 issn: 0025-3227 Marine Geology 378: 5-19 (2016) http://hdl.handle.net/10261/135510 10.1016/j.margeo.2015.10.004 http://dx.doi.org/10.13039/501100003329 http://dx.doi.org/10.13039/501100011011 https://dx.doi.org/10.1016/j.margeo.2015.10.004 Sí none Elsevier
institution ICM ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-icm-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del ICM España
topic Gulf of Cadiz
Contourite depositional systems
Erosional features
Morphology
Seismic stratigraphy
Mediterranean Outflow Water
Gulf of Cadiz
Contourite depositional systems
Erosional features
Morphology
Seismic stratigraphy
Mediterranean Outflow Water
spellingShingle Gulf of Cadiz
Contourite depositional systems
Erosional features
Morphology
Seismic stratigraphy
Mediterranean Outflow Water
Gulf of Cadiz
Contourite depositional systems
Erosional features
Morphology
Seismic stratigraphy
Mediterranean Outflow Water
García, Marga
Hernández-Molina, Francisco J.
Alonso, Belén
Vázquez, Juan Tomás
Ercilla, Gemma
Llave, Estefanía
Casas, David
Erosive sub-circular depressions on the Guadalquivir Bank (Gulf of Cadiz): Interaction between bottom current, mass-wasting and tectonic processes
description Special issue The contourite log-book: significance for palaeoceanography, ecosystems and slope instability.-- 15 pages, 9 figures
author2 Ministerio de Economía y Competitividad (España)
author_facet Ministerio de Economía y Competitividad (España)
García, Marga
Hernández-Molina, Francisco J.
Alonso, Belén
Vázquez, Juan Tomás
Ercilla, Gemma
Llave, Estefanía
Casas, David
format artículo
topic_facet Gulf of Cadiz
Contourite depositional systems
Erosional features
Morphology
Seismic stratigraphy
Mediterranean Outflow Water
author García, Marga
Hernández-Molina, Francisco J.
Alonso, Belén
Vázquez, Juan Tomás
Ercilla, Gemma
Llave, Estefanía
Casas, David
author_sort García, Marga
title Erosive sub-circular depressions on the Guadalquivir Bank (Gulf of Cadiz): Interaction between bottom current, mass-wasting and tectonic processes
title_short Erosive sub-circular depressions on the Guadalquivir Bank (Gulf of Cadiz): Interaction between bottom current, mass-wasting and tectonic processes
title_full Erosive sub-circular depressions on the Guadalquivir Bank (Gulf of Cadiz): Interaction between bottom current, mass-wasting and tectonic processes
title_fullStr Erosive sub-circular depressions on the Guadalquivir Bank (Gulf of Cadiz): Interaction between bottom current, mass-wasting and tectonic processes
title_full_unstemmed Erosive sub-circular depressions on the Guadalquivir Bank (Gulf of Cadiz): Interaction between bottom current, mass-wasting and tectonic processes
title_sort erosive sub-circular depressions on the guadalquivir bank (gulf of cadiz): interaction between bottom current, mass-wasting and tectonic processes
publisher Elsevier
publishDate 2016-08
url http://hdl.handle.net/10261/135510
http://dx.doi.org/10.13039/501100003329
http://dx.doi.org/10.13039/501100011011
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