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Comptes Rendus Géoscience
Volume 336, n° 2
pages 169-170 (février 2004)
Doi : 10.1016/j.crte.2003.12.001
Commentaire à la note de Cristian Desreumaux et al. intitulée Découverte de turbidites du Crétacé supérieur métamorphisées au contact d'intrusions d'ophites dans les Pyrénées occidentales (vallée d'Aspe, France). Vers une révision de l'âge des ophites pyrénéennes
[C. R. Geoscience 334 (2002) 197]

Bernard  Azambre a * ,  Michel  Rossy b ,  Gérard  Bossière c
aDépartement de pétrologie, université Pierre-et-Marie-Curie, 4, place Jussieu, 75252 Paris cedex 05, France 
bDépartement de géosciences (EA 2642), université de Franche-Comté, route de Gray, 25030 Besançon cedex, France 
cLaboratoire de planétologie et géodynamique (UMR CNRS 6112), 2, rue de la Houssinière, BP 92208, 44322 Nantes cedex 3, France 

*Auteur correspondant.

© 2003  Académie des sciences@@#104156@@

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