Deep reflection seismic imaging of the internal zone of the South Armorican Hercynian belt (western France) (ARMOR 2/Géofrance 3D Program)

[1]  J. Brun,et al.  Late pervasive crustal-scale extension in the south Armorican Hercynian belt (Vendée, France) , 2004 .

[2]  C. Truffert,et al.  Imagerie sismique de la zone de collision hercynienne dans le Sud-Est du Massif armoricain (projet Armor 2/programme Géofrance 3D) , 2003 .

[3]  M. Ballèvre,et al.  Ductile Thrusting Recorded by the Garnet Isograd from Blueschist-Facies Metapelites of the Ile de Groix, Armorican Massif, France , 2002 .

[4]  M. Brown,et al.  Rapid Variscan exhumation and the role of magma in core complex formation: southern Brittany metamorphic belt, France , 1996 .

[5]  K. A. Jones,et al.  High‐temperature ‘clockwise’P‐T paths and melting in the development of regional migmatites: an example from southern Brittany, France , 1990 .

[6]  C. Audren,et al.  Controls on P–T–t deformation path from amphibole zonation during progressive metamorphism of basic rocks (estuary of the River Vilaine, South Brittany, France) , 1988 .

[7]  J. Brun,et al.  Combined thrusting and wrenching in the Ibero-Armorican arc: A corner effect during continental collision , 1982 .

[8]  D. Gapais,et al.  Les « Porphyroı̈des » de Bretagne méridionale : une unité de HP–BT dans la chaı̂ne hercynienne , 2002 .

[9]  G. Godard The Les Essarts eclogite-bearing metamorphic Complex (Vendée, southern Armorican Massif, France): , 2001 .

[10]  J. V. D. Driessche,et al.  La zone de cisaillement de Quiberon : témoin d'extension de la chaîne varisque en Bretagne méridionale au Carbonifére , 1993 .

[11]  A. Vauchez,et al.  Strain and deformation mechanisms in the Variscan nappes of Vendée, South Brittany, France , 1987 .

[12]  P. Jégouzo The South Armorican Shear Zone , 1980 .

[13]  J. Brun,et al.  Signification des variations et anomalies de la deformation dans un segment de la chaine hercynienne (les series cristallophylliennes de la Vendee littorale, Massif armoricain) , 1976 .