Iberian plate kinematics and Alpine collision in the Pyrenees

With the aim to unravel first-order motions associated with the Alpine collisional history of the Pyrenees in SW Europe, we perform a plate-kinematic analysis of Iberia motion since the latest Mesozoic in a six-plate circuit. This analysis leads to reconstructions of the North Atlantic for the lates...

Full description

Bibliographic Details
Main Authors: Vissers, R.L.M., Meijer, P.Th.
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://dspace.library.uu.nl/handle/1874/258835
id ftunivutrecht:oai:dspace.library.uu.nl:1874/258835
record_format openpolar
spelling ftunivutrecht:oai:dspace.library.uu.nl:1874/258835 2023-07-23T04:20:41+02:00 Iberian plate kinematics and Alpine collision in the Pyrenees Vissers, R.L.M. Meijer, P.Th. 2012 image/pdf https://dspace.library.uu.nl/handle/1874/258835 en eng 0012-8252 https://dspace.library.uu.nl/handle/1874/258835 info:eu-repo/semantics/ClosedAccess Aardwetenschappen Plate kinematics Iberia Pyrenees Article 2012 ftunivutrecht 2023-07-02T00:34:43Z With the aim to unravel first-order motions associated with the Alpine collisional history of the Pyrenees in SW Europe, we perform a plate-kinematic analysis of Iberia motion since the latest Mesozoic in a six-plate circuit. This analysis leads to reconstructions of the North Atlantic for the latest Cretaceous well in line with previous studies and supported by onland paleomagnetic data. Our study, moreover, shows that for each of the magnetic anomalies studied, a combination exists of total reconstruction poles for the different plates and plate fragments such that the modeled shortening values in the Pyrenees are in good agreement with the shortening values inferred from partially restored sections of the balanced ECORS Pyrenees profile. At the same time, the magnitude of the belt-averaged shear, i.e., the strike-slip component divided by the normal shortening, is predicted to be smaller than implicit in previous plate-kinematic studies, which seems consistent with the generally recognized thrust-belt nature of the Pyrenees. Our analysis yields a set of preferred total reconstruction poles for each of the plates and plate fragments. Using these poles, a net Africa–Iberia motion path is calculated that can be used as an independent constraint on the geodynamics of the western Mediterranean region. Article in Journal/Newspaper North Atlantic Utrecht University Repository
institution Open Polar
collection Utrecht University Repository
op_collection_id ftunivutrecht
language English
topic Aardwetenschappen
Plate kinematics
Iberia
Pyrenees
spellingShingle Aardwetenschappen
Plate kinematics
Iberia
Pyrenees
Vissers, R.L.M.
Meijer, P.Th.
Iberian plate kinematics and Alpine collision in the Pyrenees
topic_facet Aardwetenschappen
Plate kinematics
Iberia
Pyrenees
description With the aim to unravel first-order motions associated with the Alpine collisional history of the Pyrenees in SW Europe, we perform a plate-kinematic analysis of Iberia motion since the latest Mesozoic in a six-plate circuit. This analysis leads to reconstructions of the North Atlantic for the latest Cretaceous well in line with previous studies and supported by onland paleomagnetic data. Our study, moreover, shows that for each of the magnetic anomalies studied, a combination exists of total reconstruction poles for the different plates and plate fragments such that the modeled shortening values in the Pyrenees are in good agreement with the shortening values inferred from partially restored sections of the balanced ECORS Pyrenees profile. At the same time, the magnitude of the belt-averaged shear, i.e., the strike-slip component divided by the normal shortening, is predicted to be smaller than implicit in previous plate-kinematic studies, which seems consistent with the generally recognized thrust-belt nature of the Pyrenees. Our analysis yields a set of preferred total reconstruction poles for each of the plates and plate fragments. Using these poles, a net Africa–Iberia motion path is calculated that can be used as an independent constraint on the geodynamics of the western Mediterranean region.
format Article in Journal/Newspaper
author Vissers, R.L.M.
Meijer, P.Th.
author_facet Vissers, R.L.M.
Meijer, P.Th.
author_sort Vissers, R.L.M.
title Iberian plate kinematics and Alpine collision in the Pyrenees
title_short Iberian plate kinematics and Alpine collision in the Pyrenees
title_full Iberian plate kinematics and Alpine collision in the Pyrenees
title_fullStr Iberian plate kinematics and Alpine collision in the Pyrenees
title_full_unstemmed Iberian plate kinematics and Alpine collision in the Pyrenees
title_sort iberian plate kinematics and alpine collision in the pyrenees
publishDate 2012
url https://dspace.library.uu.nl/handle/1874/258835
genre North Atlantic
genre_facet North Atlantic
op_relation 0012-8252
https://dspace.library.uu.nl/handle/1874/258835
op_rights info:eu-repo/semantics/ClosedAccess
_version_ 1772185301632942080