1 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 SSW-NNE 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)...

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Main Authors: Enzo Mantovani, Marcello Viti, Daniele Babbucci, Dario Albarello
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.563.1981
http://www.earth-prints.org/bitstream/2122/2071/1/Nubia Eurasia_Mantovani.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.563.1981 2023-05-15T17:28:21+02:00 1 Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence Enzo Mantovani Marcello Viti Daniele Babbucci Dario Albarello The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.563.1981 http://www.earth-prints.org/bitstream/2122/2071/1/Nubia Eurasia_Mantovani.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.563.1981 http://www.earth-prints.org/bitstream/2122/2071/1/Nubia Eurasia_Mantovani.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.earth-prints.org/bitstream/2122/2071/1/Nubia Eurasia_Mantovani.pdf Key words Nubia-Eurasia kinematics- Mediterranean region – Plio-Quaternary deformation text ftciteseerx 2016-01-08T12:08:16Z It is argued that the Plio-Quaternary deformation pattern in the Mediterranean region is compatible with a SSW-NNE 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 the reason 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. Text North Atlantic Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Key words
Nubia-Eurasia kinematics- Mediterranean region – Plio-Quaternary deformation
spellingShingle Key words
Nubia-Eurasia kinematics- Mediterranean region – Plio-Quaternary deformation
Enzo Mantovani
Marcello Viti
Daniele Babbucci
Dario Albarello
1 Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence
topic_facet Key words
Nubia-Eurasia kinematics- Mediterranean region – Plio-Quaternary deformation
description It is argued that the Plio-Quaternary deformation pattern in the Mediterranean region is compatible with a SSW-NNE 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 the reason 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.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Enzo Mantovani
Marcello Viti
Daniele Babbucci
Dario Albarello
author_facet Enzo Mantovani
Marcello Viti
Daniele Babbucci
Dario Albarello
author_sort Enzo Mantovani
title 1 Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence
title_short 1 Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence
title_full 1 Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence
title_fullStr 1 Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence
title_full_unstemmed 1 Nubia-Eurasia kinematics: an alternative interpretation from Mediterranean and North Atlantic evidence
title_sort 1 nubia-eurasia kinematics: an alternative interpretation from mediterranean and north atlantic evidence
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.563.1981
http://www.earth-prints.org/bitstream/2122/2071/1/Nubia Eurasia_Mantovani.pdf
genre North Atlantic
genre_facet North Atlantic
op_source http://www.earth-prints.org/bitstream/2122/2071/1/Nubia Eurasia_Mantovani.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.563.1981
http://www.earth-prints.org/bitstream/2122/2071/1/Nubia Eurasia_Mantovani.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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