Articles | Volume 6, issue 2
https://doi.org/10.5194/se-6-643-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-6-643-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
High-temperature metamorphism during extreme thinning of the continental crust: a reappraisal of the North Pyrenean passive paleomargin
C. Clerc
CORRESPONDING AUTHOR
Laboratoire de Géologie, CNRS-UMR8538, Ecole normale supérieure, 24 rue Lhomond, 75231 Paris, France
Géosciences Montpellier, CNRS-UMR 5243, Université de Montpellier 2, Place Eugène Bataillon, 34095 Montpellier, France
now at: ISTO, 1A rue de la Férollerie, 45100 Orléans, France
Invited contribution by C. Clerc, recipient of the EGU Outstanding Student Poster (OSP) Award 2012.
A. Lahfid
BRGM/ISTO, 3 avenue Claude Guillemin, 45000 Orléans, France
P. Monié
Géosciences Montpellier, CNRS-UMR 5243, Université de Montpellier 2, Place Eugène Bataillon, 34095 Montpellier, France
Y. Lagabrielle
Géosciences Rennes, UMR 6118, Université Rennes 1, Campus de Beaulieu, 35042 Rennes, France
C. Chopin
Laboratoire de Géologie, CNRS-UMR8538, Ecole normale supérieure, 24 rue Lhomond, 75231 Paris, France
M. Poujol
Géosciences Rennes, UMR 6118, Université Rennes 1, Campus de Beaulieu, 35042 Rennes, France
P. Boulvais
Géosciences Rennes, UMR 6118, Université Rennes 1, Campus de Beaulieu, 35042 Rennes, France
J.-C. Ringenbach
TOTAL, CSTJF, avenue Larribau, 64000 Pau, France
E. Masini
TOTAL, CSTJF, avenue Larribau, 64000 Pau, France
M. de St Blanquat
GET, 14 avenue Edouard Belin, 31400 Toulouse, France
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75 citations as recorded by crossref.
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Short summary
The northern flank of the Pyrenean belt is an example of an inverted hot passive margin. We provide a data set of more than 100 peak-temperature estimates by RSCM and 18 new radiogenic ages from metamorphic and magmatic rocks from the North Pyrenean Zone. The results indicate a first-order control of the thermal gradient by the intensity of the Cretaceous crustal thinning. The highest grades of metamorphism are associated with the areas where mantle peridotites have been unroofed or exhumed.
The northern flank of the Pyrenean belt is an example of an inverted hot passive margin. We...