Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea

Rui, L. . et al.-- Final Conference ARCA PROJECT : ARctic: present Climatic change and pAst extreme events, 11 October, 2016, Rome.-- 3 pages, 3 figures The development of high latitude continental margin has been mainly controlled by glacigenic processes during the glacial maxima. Superimposed to t...

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Main Authors: Rui, L., Urgeles, Roger, Accettella, Daniela
Format: Conference Object
Language:unknown
Published: 2016
Subjects:
Arctic
Barents Sea
Online Access:http://hdl.handle.net/10261/171441
id ftcsic:oai:digital.csic.es:10261/171441
record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/171441 2024-02-11T09:59:14+01:00 Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea Rui, L. Urgeles, Roger Accettella, Daniela 2016-10-11 http://hdl.handle.net/10261/171441 unknown http://www.arcaproject.it/index.php/en/results Sí ARCA PROJECT : ARctic: present Climatic change and pAst extreme events : Final Conference (2016) http://hdl.handle.net/10261/171441 open comunicación de congreso http://purl.org/coar/resource_type/c_5794 2016 ftcsic 2024-01-16T10:33:40Z Rui, L. . et al.-- Final Conference ARCA PROJECT : ARctic: present Climatic change and pAst extreme events, 11 October, 2016, Rome.-- 3 pages, 3 figures The development of high latitude continental margin has been mainly controlled by glacigenic processes during the glacial maxima. Superimposed to these, there are both downslope and alongslope sedimentary processes (turbidites and contourites). [.] Peer Reviewed Conference Object Arctic Arctic Barents Sea Digital.CSIC (Spanish National Research Council) Arctic Barents Sea
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language unknown
description Rui, L. . et al.-- Final Conference ARCA PROJECT : ARctic: present Climatic change and pAst extreme events, 11 October, 2016, Rome.-- 3 pages, 3 figures The development of high latitude continental margin has been mainly controlled by glacigenic processes during the glacial maxima. Superimposed to these, there are both downslope and alongslope sedimentary processes (turbidites and contourites). [.] Peer Reviewed
format Conference Object
author Rui, L.
Urgeles, Roger
Accettella, Daniela
spellingShingle Rui, L.
Urgeles, Roger
Accettella, Daniela
Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea
author_facet Rui, L.
Urgeles, Roger
Accettella, Daniela
author_sort Rui, L.
title Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea
title_short Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea
title_full Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea
title_fullStr Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea
title_full_unstemmed Downslope and alongslope sedimentary processes on a high latitude continental margin: NW Barents Sea
title_sort downslope and alongslope sedimentary processes on a high latitude continental margin: nw barents sea
publishDate 2016
url http://hdl.handle.net/10261/171441
geographic Arctic
Barents Sea
geographic_facet Arctic
Barents Sea
genre Arctic
Arctic
Barents Sea
genre_facet Arctic
Arctic
Barents Sea
op_relation http://www.arcaproject.it/index.php/en/results
Sí
ARCA PROJECT : ARctic: present Climatic change and pAst extreme events : Final Conference (2016)
http://hdl.handle.net/10261/171441
op_rights open
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