Magnetic anomalies of the NW Iberian continental margin and the adjacent abyssal plains

The NW Iberian margin is a hyperextended continental margin, formed during the opening of the North Atlantic Ocean, where a subsequent partial tectonic inversion has undergone during the Alpine Orogeny. This succession of tectonic episodes determines the magnetic signature of the margin. The Spanish...

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Published in:Journal of Maps
Main Authors: María Druet, Manuel Catalán, José Martín-Dávila, Yasmina M. Martos, Alfonso Muñoz-Martín, José Luis Granja-Bruña, Adolfo Maestro
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis Group 2020
Subjects:
Online Access:https://doi.org/10.1080/17445647.2020.1806123
https://doaj.org/article/1fba52dd3bb9471ba5b39e5b43938976
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spelling ftdoajarticles:oai:doaj.org/article:1fba52dd3bb9471ba5b39e5b43938976 2023-05-15T17:32:45+02:00 Magnetic anomalies of the NW Iberian continental margin and the adjacent abyssal plains María Druet Manuel Catalán José Martín-Dávila Yasmina M. Martos Alfonso Muñoz-Martín José Luis Granja-Bruña Adolfo Maestro 2020-12-01T00:00:00Z https://doi.org/10.1080/17445647.2020.1806123 https://doaj.org/article/1fba52dd3bb9471ba5b39e5b43938976 EN eng Taylor & Francis Group http://dx.doi.org/10.1080/17445647.2020.1806123 https://doaj.org/toc/1744-5647 1744-5647 doi:10.1080/17445647.2020.1806123 https://doaj.org/article/1fba52dd3bb9471ba5b39e5b43938976 Journal of Maps, Vol 16, Iss 2, Pp 680-688 (2020) geomagnetism nw iberia ne atlantic ocean magnetic anomalies Maps G3180-9980 article 2020 ftdoajarticles https://doi.org/10.1080/17445647.2020.1806123 2022-12-31T15:30:45Z The NW Iberian margin is a hyperextended continental margin, formed during the opening of the North Atlantic Ocean, where a subsequent partial tectonic inversion has undergone during the Alpine Orogeny. This succession of tectonic episodes determines the magnetic signature of the margin. The Spanish Exclusive Economic Zone Project has carried out seven one-month cruises between 2001 and 2009. To extend and densify the spatial coverage, we have used data from the World Digital Magnetic Anomaly Map. Here, we describe the methodology used for the acquisition and data processing of the magnetic field data. The use of diverse instrumentation, a non-complete external field’s cancelation, and the use of different magnetic core field models, contributed to the total error budget. To reduce it, we have used a leveling algorithm which minimizes all these contributions. Finally, a statistical analysis was applied using crossover residuals, showing a resolution better than 28 nT. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Journal of Maps 16 2 680 688
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic geomagnetism
nw iberia
ne atlantic ocean
magnetic anomalies
Maps
G3180-9980
spellingShingle geomagnetism
nw iberia
ne atlantic ocean
magnetic anomalies
Maps
G3180-9980
María Druet
Manuel Catalán
José Martín-Dávila
Yasmina M. Martos
Alfonso Muñoz-Martín
José Luis Granja-Bruña
Adolfo Maestro
Magnetic anomalies of the NW Iberian continental margin and the adjacent abyssal plains
topic_facet geomagnetism
nw iberia
ne atlantic ocean
magnetic anomalies
Maps
G3180-9980
description The NW Iberian margin is a hyperextended continental margin, formed during the opening of the North Atlantic Ocean, where a subsequent partial tectonic inversion has undergone during the Alpine Orogeny. This succession of tectonic episodes determines the magnetic signature of the margin. The Spanish Exclusive Economic Zone Project has carried out seven one-month cruises between 2001 and 2009. To extend and densify the spatial coverage, we have used data from the World Digital Magnetic Anomaly Map. Here, we describe the methodology used for the acquisition and data processing of the magnetic field data. The use of diverse instrumentation, a non-complete external field’s cancelation, and the use of different magnetic core field models, contributed to the total error budget. To reduce it, we have used a leveling algorithm which minimizes all these contributions. Finally, a statistical analysis was applied using crossover residuals, showing a resolution better than 28 nT.
format Article in Journal/Newspaper
author María Druet
Manuel Catalán
José Martín-Dávila
Yasmina M. Martos
Alfonso Muñoz-Martín
José Luis Granja-Bruña
Adolfo Maestro
author_facet María Druet
Manuel Catalán
José Martín-Dávila
Yasmina M. Martos
Alfonso Muñoz-Martín
José Luis Granja-Bruña
Adolfo Maestro
author_sort María Druet
title Magnetic anomalies of the NW Iberian continental margin and the adjacent abyssal plains
title_short Magnetic anomalies of the NW Iberian continental margin and the adjacent abyssal plains
title_full Magnetic anomalies of the NW Iberian continental margin and the adjacent abyssal plains
title_fullStr Magnetic anomalies of the NW Iberian continental margin and the adjacent abyssal plains
title_full_unstemmed Magnetic anomalies of the NW Iberian continental margin and the adjacent abyssal plains
title_sort magnetic anomalies of the nw iberian continental margin and the adjacent abyssal plains
publisher Taylor & Francis Group
publishDate 2020
url https://doi.org/10.1080/17445647.2020.1806123
https://doaj.org/article/1fba52dd3bb9471ba5b39e5b43938976
genre North Atlantic
genre_facet North Atlantic
op_source Journal of Maps, Vol 16, Iss 2, Pp 680-688 (2020)
op_relation http://dx.doi.org/10.1080/17445647.2020.1806123
https://doaj.org/toc/1744-5647
1744-5647
doi:10.1080/17445647.2020.1806123
https://doaj.org/article/1fba52dd3bb9471ba5b39e5b43938976
op_doi https://doi.org/10.1080/17445647.2020.1806123
container_title Journal of Maps
container_volume 16
container_issue 2
container_start_page 680
op_container_end_page 688
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