Ar Study of Oceanic and Continental Deformation Processes During An
A(40)Ar/(39) Ar study of oceanic and continental deformation processes during an oblique collision: Taconian orogeny in the Quebec reentrant of the Canadian Appalachians Michel Malo, Gilles Ruffet, Alix Pincivy, Alain Tremblay To cite this version: Michel Malo, Gilles Ruffet, Alix Pincivy, Alain Tremblay. A(40)Ar/(39) Ar study of oceanic and continental deformation processes during an oblique collision: Taconian orogeny in the Quebec reen- trant of the Canadian Appalachians. Tectonics, American Geophysical Union (AGU), 2008, 27 (4), pp.TC4001. 10.1029/2006TC002094. insu-00322674 HAL Id: insu-00322674 https://hal-insu.archives-ouvertes.fr/insu-00322674 Submitted on 29 Jun 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. TECTONICS, VOL. 27, TC4001, doi:10.1029/2006TC002094, 2008 A 40Ar/39Ar study of oceanic and continental deformation processes during an oblique collision: Taconian orogeny in the Quebec reentrant of the Canadian Appalachians Michel Malo,1 Gilles Ruffet,2 Alix Pincivy,1 and Alain Tremblay3 Received 7 December 2006; revised 9 January 2008; accepted 10 March 2008; published 1 July 2008. [1] Two phases of penetrative deformation are Stockmal et al., 1987; Malo et al., 1995; van Staal et documented in the Taconian hinterland of the al., 1998], particularly for the Ordovician Taconian orogeny Appalachian orogen in the Gaspe´ Peninsula.
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