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Comptes Rendus Géoscience
Volume 336, n° 2
pages 171-172 (février 2004)
Doi : 10.1016/j.crte.2003.11.002
Commentaire à la note de Christian 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]

Cédric  Rapaille a ,  Hervé  Bertrand b * ,  Andrea  Marzoli ac
aSection des Sciences de la Terre, université de Genève, 13, rue des Maraîchers, 1205 Genève, Suisse 
bLaboratoire des Sciences de la Terre, UMR-CNRS 5570, École normale supérieure de Lyon et université Lyon-1, 46 allée d'Italie, 69364 Lyon cedex 07, France 
cDipartimento di Mineralogia e Petrologia, Università di Padova, Corso Garibaldi 37, 35137 Padova, Italie 

*Auteur correspondant.



© 2003  Académie des sciences@@#104156@@

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