Textural characteristics and facies of sand‐rich contourite depositional systems
Brackenridge, Rachel E. ... et al.-- 30 pages, 14 figures, 2 tables
| Authors: | , , |
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| Format: | article |
| Publication Date: | 2018 |
| Country: | España |
| Institution: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repository: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/172929 |
| Online Access: | http://hdl.handle.net/10261/172929 |
| Access Level: | Open access |
| Keyword: | Grain size Contourites Sediment facies model Gulf of Cadiz Deep-water sands |
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Textural characteristics and facies of sand‐rich contourite depositional systemsBrackenridge, Rachel E.Ercilla, GemmaFrancés, GuillermoGrain sizeContouritesSediment facies modelGulf of CadizDeep-water sandsBrackenridge, Rachel E. ... et al.-- 30 pages, 14 figures, 2 tablesThis work presents a detailed study of CONTOURIBER and Integrated Ocean Drilling Program 339 sediment data targeting sand‐rich contourites in the Eastern Gulf of Cadiz. All of the collected sediments are interpreted as contourites (deposited or reworked by bottom currents) on the basis of oceanographic setting, seismic and morphometric features, and facies characteristics. A variety of sandy and associated facies are found across the study area including: (i) bioturbated muddy contourites; (ii) mottled silty contourites; (iii) very fine mottled and fine‐grained bioturbated sandy contourites; (iv) massive and laminated sandy contourites; and (v) coarse sandy/gravel contourites. The thickest sands occur within contourite channels and there is a marked reduction in sand content laterally away from channels. Complementary to the facies descriptions, grain‐size analysis of 675 samples reveals distinctive trends in textural properties linked to depositional processes under the action of bottom currents. The finest muddy contourites (<20 μm) show normal grain‐size distributions, poor to very poor sorting, and zero or low skewness. These are deposited by settling from weak bottom currents with a fine suspension load. Muddy to fine sandy contourites (20 to 200 μm) trend towards better sorting and initially finer and then coarser skew. These are typical depositional trends for contourites. As current velocity and carrying capacity increase, more of the finest fraction remains in suspension and bedload transport becomes more important. Clean sandy contourites (>200 μm) are better sorted. They result from the action of dominant bedload transport and winnowing at high current speeds. The results highlight the importance of bottom current velocity, sediment supply and bioturbational mixing in controlling contourite facies. Despite growing interest in their hydrocarbon exploration potential, contourite sands have remained poorly understood. This research therefore has important implications for developing current understanding of these deposits and aiding the correct interpretation of deep marine sands and depositional processesThis research formed part of the lead author's PhD programme at Heriot‐Watt University, supported by an Ali Danesh Scholarship and of the Masters by research from Claudia Jones in the Department of Earth Sciences of the Royal Holloway University of London. The research was also partially supported through the Spanish Ciencia y Tecnologías Marinas projects CTM 2012‐39599‐C03, CGL2016‐80445‐R, and CTM2016‐75129‐C3‐1‐R, and conducted in the framework of ‘The Drifters’ Research Group of the Royal Holloway University of London (RHUL)Peer ReviewedInternational Association of SedimentologistsUniversity of LondonMinisterio de Economía y Competitividad (España)Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]2018201820182018info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501http://hdl.handle.net/10261/172929reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Ingléshttps://doi.org/10.1111/sed.12463Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/1729292026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
Textural characteristics and facies of sand‐rich contourite depositional systems |
| title |
Textural characteristics and facies of sand‐rich contourite depositional systems |
| spellingShingle |
Textural characteristics and facies of sand‐rich contourite depositional systems Brackenridge, Rachel E. Grain size Contourites Sediment facies model Gulf of Cadiz Deep-water sands |
| title_short |
Textural characteristics and facies of sand‐rich contourite depositional systems |
| title_full |
Textural characteristics and facies of sand‐rich contourite depositional systems |
| title_fullStr |
Textural characteristics and facies of sand‐rich contourite depositional systems |
| title_full_unstemmed |
Textural characteristics and facies of sand‐rich contourite depositional systems |
| title_sort |
Textural characteristics and facies of sand‐rich contourite depositional systems |
| dc.creator.none.fl_str_mv |
Brackenridge, Rachel E. Ercilla, Gemma Francés, Guillermo |
| author |
Brackenridge, Rachel E. |
| author_facet |
Brackenridge, Rachel E. Ercilla, Gemma Francés, Guillermo |
| author_role |
author |
| author2 |
Ercilla, Gemma Francés, Guillermo |
| author2_role |
author author |
| dc.contributor.none.fl_str_mv |
University of London Ministerio de Economía y Competitividad (España) Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] |
| dc.subject.none.fl_str_mv |
Grain size Contourites Sediment facies model Gulf of Cadiz Deep-water sands |
| topic |
Grain size Contourites Sediment facies model Gulf of Cadiz Deep-water sands |
| description |
Brackenridge, Rachel E. ... et al.-- 30 pages, 14 figures, 2 tables |
| publishDate |
2018 |
| dc.date.none.fl_str_mv |
2018 2018 2018 2018 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 |
| format |
article |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/172929 |
| url |
http://hdl.handle.net/10261/172929 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
https://doi.org/10.1111/sed.12463 Sí |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
International Association of Sedimentologists |
| publisher.none.fl_str_mv |
International Association of Sedimentologists |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
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Consejo Superior de Investigaciones Científicas (CSIC) |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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DIGITAL.CSIC. Repositorio Institucional del CSIC |
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1869416144641720320 |
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15,812429 |