Asymmetric Atlantic continental margins
We analyze the gross crustal structure of the Atlantic Ocean passive continental margins from north to the south, comparing eleven sections of the conjugate margins. As a general result, the western margins show a sharper continental-ocean transition with respect to the eastern margins that rather s...
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ftdoajarticles:oai:doaj.org/article:171e1bc5968142c5b708b2671b35ed1b 2023-10-01T03:56:21+02:00 Asymmetric Atlantic continental margins Adriano Vangone Carlo Doglioni 2021-09-01T00:00:00Z https://doi.org/10.1016/j.gsf.2021.101205 https://doaj.org/article/171e1bc5968142c5b708b2671b35ed1b EN eng Elsevier http://www.sciencedirect.com/science/article/pii/S1674987121000694 https://doaj.org/toc/1674-9871 1674-9871 doi:10.1016/j.gsf.2021.101205 https://doaj.org/article/171e1bc5968142c5b708b2671b35ed1b Geoscience Frontiers, Vol 12, Iss 5, Pp 101205- (2021) Passive continental margin Asymmetric rift Moho dip Continental-ocean transition Westward drift of the lithosphere Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.1016/j.gsf.2021.101205 2023-09-03T00:37:03Z We analyze the gross crustal structure of the Atlantic Ocean passive continental margins from north to the south, comparing eleven sections of the conjugate margins. As a general result, the western margins show a sharper continental-ocean transition with respect to the eastern margins that rather show a wider stretched and thinner margin. The Moho is in average about 5.7°±1° dipping toward the interior of the continent on the western side, whereas it is about 2.7°±1° in the eastern margins. Moreover, the stretched continental crust is on average 244 km wide on the western side, whereas it is up to about 439 km on the eastern side of the Atlantic. This systematic asymmetry reflects the early stages of the diachronous Mesozoic to Cenozoic continental rifting, which is inferred as the result of a polarized westward motion of both western and eastern plates, being Greenland, Northern and Southern Americas plates moving westward faster with respect to Scandinavia, Europe and Africa, relative to the underlying mantle. Article in Journal/Newspaper Greenland Directory of Open Access Journals: DOAJ Articles Greenland Geoscience Frontiers 12 5 101205 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Passive continental margin Asymmetric rift Moho dip Continental-ocean transition Westward drift of the lithosphere Geology QE1-996.5 |
spellingShingle |
Passive continental margin Asymmetric rift Moho dip Continental-ocean transition Westward drift of the lithosphere Geology QE1-996.5 Adriano Vangone Carlo Doglioni Asymmetric Atlantic continental margins |
topic_facet |
Passive continental margin Asymmetric rift Moho dip Continental-ocean transition Westward drift of the lithosphere Geology QE1-996.5 |
description |
We analyze the gross crustal structure of the Atlantic Ocean passive continental margins from north to the south, comparing eleven sections of the conjugate margins. As a general result, the western margins show a sharper continental-ocean transition with respect to the eastern margins that rather show a wider stretched and thinner margin. The Moho is in average about 5.7°±1° dipping toward the interior of the continent on the western side, whereas it is about 2.7°±1° in the eastern margins. Moreover, the stretched continental crust is on average 244 km wide on the western side, whereas it is up to about 439 km on the eastern side of the Atlantic. This systematic asymmetry reflects the early stages of the diachronous Mesozoic to Cenozoic continental rifting, which is inferred as the result of a polarized westward motion of both western and eastern plates, being Greenland, Northern and Southern Americas plates moving westward faster with respect to Scandinavia, Europe and Africa, relative to the underlying mantle. |
format |
Article in Journal/Newspaper |
author |
Adriano Vangone Carlo Doglioni |
author_facet |
Adriano Vangone Carlo Doglioni |
author_sort |
Adriano Vangone |
title |
Asymmetric Atlantic continental margins |
title_short |
Asymmetric Atlantic continental margins |
title_full |
Asymmetric Atlantic continental margins |
title_fullStr |
Asymmetric Atlantic continental margins |
title_full_unstemmed |
Asymmetric Atlantic continental margins |
title_sort |
asymmetric atlantic continental margins |
publisher |
Elsevier |
publishDate |
2021 |
url |
https://doi.org/10.1016/j.gsf.2021.101205 https://doaj.org/article/171e1bc5968142c5b708b2671b35ed1b |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland |
genre_facet |
Greenland |
op_source |
Geoscience Frontiers, Vol 12, Iss 5, Pp 101205- (2021) |
op_relation |
http://www.sciencedirect.com/science/article/pii/S1674987121000694 https://doaj.org/toc/1674-9871 1674-9871 doi:10.1016/j.gsf.2021.101205 https://doaj.org/article/171e1bc5968142c5b708b2671b35ed1b |
op_doi |
https://doi.org/10.1016/j.gsf.2021.101205 |
container_title |
Geoscience Frontiers |
container_volume |
12 |
container_issue |
5 |
container_start_page |
101205 |
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1778525818972012544 |