Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence
It is argued that the Plio-Quaternary deformation pattern in the Mediterranean region is compatible with a SSWNNE convergence between Africa (Nubia) and Eurasia and that the significant difference between this kinematics and the one provided by global models (SSE-NNW convergence e.g., the NUVEL-1) m...
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Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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ftdoajarticles:oai:doaj.org/article:60e7013078aa4842a7319fba85b8816c 2023-05-15T17:28:32+02:00 Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence D. Albarello D. Babbucci M. Viti E. Mantovani 2007-06-01T00:00:00Z https://doi.org/10.4401/ag-3073 https://doaj.org/article/60e7013078aa4842a7319fba85b8816c EN eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) http://www.annalsofgeophysics.eu/index.php/annals/article/view/3073 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X doi:10.4401/ag-3073 1593-5213 2037-416X https://doaj.org/article/60e7013078aa4842a7319fba85b8816c Annals of Geophysics, Vol 50, Iss 3 (2007) Nubia-Eurasia kinematics Mediterranean region Plio-Quaternary deformation Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 article 2007 ftdoajarticles https://doi.org/10.4401/ag-3073 2022-12-31T10:52:36Z It is argued that the Plio-Quaternary deformation pattern in the Mediterranean region is compatible with a SSWNNE convergence between Africa (Nubia) and Eurasia and that the significant difference between this kinematics and the one provided by global models (SSE-NNW convergence e.g., the NUVEL-1) may be due to the fact that those models interpret North Atlantic data by adopting an oversimplified two-plate configuration, which cannot account for the occurrence of significant seismotectonic activity inside the presumed Nubia and Eurasia blocks. It is shown that the adoption of a new plate configuration involving the Iberia and Morocco microplates, strongly suggested by geological and seismotectonic evidence, makes it possible to identify a kinematic model compatible within errors with the constraints recognized in the Mediterranean region and with the NUVEL-1 North Atlantic data set. Some considerations are made about why the present-day Nubia-Eurasia kinematic models inferred from geodetic observations are significantly different from long-term models, such as model NUVEL- 1 and the one proposed in this work. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Annals of Geophysics 50 3 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Nubia-Eurasia kinematics Mediterranean region Plio-Quaternary deformation Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Nubia-Eurasia kinematics Mediterranean region Plio-Quaternary deformation Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 D. Albarello D. Babbucci M. Viti E. Mantovani Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence |
topic_facet |
Nubia-Eurasia kinematics Mediterranean region Plio-Quaternary deformation Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 |
description |
It is argued that the Plio-Quaternary deformation pattern in the Mediterranean region is compatible with a SSWNNE convergence between Africa (Nubia) and Eurasia and that the significant difference between this kinematics and the one provided by global models (SSE-NNW convergence e.g., the NUVEL-1) may be due to the fact that those models interpret North Atlantic data by adopting an oversimplified two-plate configuration, which cannot account for the occurrence of significant seismotectonic activity inside the presumed Nubia and Eurasia blocks. It is shown that the adoption of a new plate configuration involving the Iberia and Morocco microplates, strongly suggested by geological and seismotectonic evidence, makes it possible to identify a kinematic model compatible within errors with the constraints recognized in the Mediterranean region and with the NUVEL-1 North Atlantic data set. Some considerations are made about why the present-day Nubia-Eurasia kinematic models inferred from geodetic observations are significantly different from long-term models, such as model NUVEL- 1 and the one proposed in this work. |
format |
Article in Journal/Newspaper |
author |
D. Albarello D. Babbucci M. Viti E. Mantovani |
author_facet |
D. Albarello D. Babbucci M. Viti E. Mantovani |
author_sort |
D. Albarello |
title |
Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence |
title_short |
Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence |
title_full |
Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence |
title_fullStr |
Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence |
title_full_unstemmed |
Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence |
title_sort |
nubia-eurasia kinematics: an alternative interpretation from mediterranean and north atlantic evidence |
publisher |
Istituto Nazionale di Geofisica e Vulcanologia (INGV) |
publishDate |
2007 |
url |
https://doi.org/10.4401/ag-3073 https://doaj.org/article/60e7013078aa4842a7319fba85b8816c |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Annals of Geophysics, Vol 50, Iss 3 (2007) |
op_relation |
http://www.annalsofgeophysics.eu/index.php/annals/article/view/3073 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X doi:10.4401/ag-3073 1593-5213 2037-416X https://doaj.org/article/60e7013078aa4842a7319fba85b8816c |
op_doi |
https://doi.org/10.4401/ag-3073 |
container_title |
Annals of Geophysics |
container_volume |
50 |
container_issue |
3 |
_version_ |
1766121269393096704 |