Vandycke, Sara ; Université de Mons > Faculté Polytechnique > Géologie fondamentale et appliquée ; Université de Mons > Faculté Polytechnique > Service de Génie Minier
Haerinck, Tom
Berwouts, Isaac
Sintubin, Manuel
Haerinck, T.
Berwouts, I
Sintubin, M.
Language :
English
Title :
Antithetic-dominated relics of the immature stage of the North-Armorican shear zone (Brittany, France)
Publication date :
27 September 2013
Journal title :
Geologica Belgica
ISSN :
1374-8505
Publisher :
Geologica Belgica, Liège, Belgium
Volume :
16
Issue :
3
Pages :
120-128
Peer reviewed :
Peer Reviewed verified by ORBi
Research unit :
F408 - Génie Minier
Research institute :
R400 - Institut de Recherche en Science et Ingénierie des Matériaux
Angelier, J., 1979. Determination of the mean principal directions of stresses for a given fault population. Tectonophysics, 56, 17-26.
Angelier, J., 1990. Inversion of feld data in fault tectonics to obtain the regional stress – III. A new rapid direct inversion method by analytical means. Geophysical Journal International, 103, 363-376.
Angelier, J., 1994. Fault slip analysis and paleostress reconstruction. In: Hancock, P. L., Continental Deformation. Pergamon Press, 53-101.
Autran, A. & Cogné J., 1980. La zone interne de l’orogène Varisque dans l’ouest de la France et sa place dans le développement de la chaîne Hercynienne. In: Cogné, J., & Slansky, M. (eds), Géologie de l’Europe du Précambrien aux bassins sédimentaires post-Hercyniens. 26è Congr. Géol. Intern., Coll C6, Paris. Mém. BRGM, 108, 90-111.
Badham, J.P.N., 1982. Strike-slip orogens: An explanation for the Hercynides. Journal of the Geological Society, London, 139, 493-504.
Bergerat, F. & Angelier J., 2008. Immature and mature transform zones near a hot spot: The South Iceland Seismic Zone and the Tjörnes Fracture Zone (Iceland). Tectonophysics, 447, 142-154.
Berthe, D., Choukroune P. & Gapais D., 1979. Orientations préférentielles du quartz et orthogneissifcation progressive en regime cissaillant: L’exemple du cissaillement sud-armoricain. Bulletin de Minéralogie, 102, 265-272.
Berwouts, I., 2011. Reconstruction of fluid system evolution in a wrench tectonic setting, Implications for the geodynamic history of Central Armorica, Brittany, France. Ph.D. thesis, Aardkundige Mededelingen, volume 26. Leuven University Press, Leuven, 253.
Brun, J.P. & Burg J.P., 1982. Combined thrusting and wrenching in the Ibero-Armoricain arc: A corner effect during continental collision. Earth and Planetary Science Letters, 61, 319-332.
Burg, J.P., Bale P., Brun J.P. & Girardeau J., 1987. Stretching lineation and transport direction in the Ibéro-Armorican arc during the siluro-devonian collision. Geodynamica Acta, Paris, 1, 1, 71-87.
Cabanis, B. et al., 1981. Carte géologique de la France a 1/50 000, feuille Morlaix (240). Bureau de Recherches Géologiques et Minières, Orléans.
Carron, J.-P., Le Guen de Kerneizon M. & Nachit H., 1994. Variscan Granites from Brittany. In: Keppie, ED. J. Pre-Mesozoic Geology in France and related areas. Springer-Verlag Berlin Heidelberg, 231-237.
Castaing, C., Rolet J., Chevremont P., Le Calvez J.Y. & Thonon P., 1987. La région de Huelgoat (Finistère central) dans le contexte géodynamique armoricain. Géologie de la France, 1, 23-36.
Chauris, L., 1969. Sur un important accident structural dans le Nord-Ouest de l’Armorique. Comptes rendus de l’Académie des Sciences, Paris, 2859-2861.
Chauris, L. & Garreau J., 1975. Les relations du granite de Guimiliau avec le Paléozoïque de la rade de Brest et du basin de Morlaix (Massif Armoricain). C. R. Acad. Sc. Paris, 280, 251-254.
Darboux, J.-R., 1991. Evolution tectonosedimentaire et structuration synmetamorphe des zones externes du segment hercynien ouest-europeen: Le Modèle du Domaine Centre Armoricain occidental. Thèse d’état, Université de Bretagne Occidentale, Brest, 267.
Deer, W. A., Howie R.A. & Zussman J., 1992. An Introduction to the rock-Forming minerals. Longman Group uk Limited, 696.
Delvaux, D. & Sperner B., 2003. New aspects of tectonic stress inversion with reference to the TENSOr program. Geological Society, London, Special publications, 212, 75-100.
Etchecopar, A., Vasseur G. & Daignieres M., 1981. An inverse problem in microtectonics for the determination of stress tensors from fault striation analysis. Journal of Structural Geology, 3, 51-65.
Faure, M., Mézeme E.B., Duguet M., Cartier C. & Talbot J.Y., 2005. Paleozoic tectonic evolution of medio-europa from the example of the french massif central and massif armorican. Journal of Virtual Explorer, 19, 1-26.
Faure, M., Sommers C., Melleton J., Cocherie A. & Lautout O., 2008. The Léon Domain (French Massif Armoricain): A westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights. International Journal of Earth Sciences, 99, 65-81.
Gapais, D. & Cobbold P.R., 1987. Slip system domains. 2. Kinematic aspects of fabric development in polycrystalline aggregates. Tectonophysics, 138, 289-309.
Garreau, J., 1983. Géomorphologie structural en Bretagne péninsulaire. La région de Morlaix. Norois, 118, 195-212.
Goré, B., Le Corre C., 1987. Cinématique hercynienne du cisaillement nord-armoricain à la bordure du granite syntectonique de Saint Renan-Kersaint (Finistère). Bulletin de la Société Géologique de France, 8, 5, 811-819.
Gumiaux, C., Judenherc S., Brun J.-P., Gapais D., Granet M. & Poupinet G., 2004. Restoration of lithosphere-scale wrenching from integrated structural and tomographic data (Hercynian belt of western France). Geology, 32, 333-336.
Kilb, D. & Rubin A.M., 2002. Implications of diverse fault orientations imaged in relocated aftershocks of the Mount Lewis, ML 5.7, California, earthquake. Journal of Geophysical Research, 107, 2294-2311.
Kim, Y.-S., Peacock D.C.P. & Sanderson D.J., 2003. Mesoscale strike-slip faults and damage zones at Marsalforn, Gozo Island, Malta. Journal of Structural Geology, 25, 793-812.
Kim, Y.-S., Peacock D.C.P. & Sanderson D.J., 2004. Fault damage zones. Journal of Structural Geology, 26, 503-517.
Lacombe, O., 2012. Do fault slip data inversions actually yield “paleostresses” that can be compared with contemporary stresses? A critical discussion. Comptes Rendus Geoscience, 344,3-4, 159-173.
Le Corre, C., Auvray B., Ballevre M. & Robardet M., 1991. Le Massif Armoricain. In: Piqué A. (éd.), Les massifs anciens de France, I. Sciences géologiquas, Strasbourg, 44, 31-104.
Matte, P., 2001. The Variscan collage and orogeny (480-290 Ma) and the tectonic definition of the Armorica microplate: A review. Terra Nova, 13, 2, 122-128.
Maussen, K., 2010. Origin and characteristics of large-scale quartz bodies along the North-Armorican shear zone, Brittany, France. Master’s thesis, Campus Library Arenberg kuLeuven, 90.
Michael, A.J., 1984. Determination of stress from slip data: Faults and folds. Journal of Geophysical Research, 89, 517-526.
Reches, Z., 1987. Determination of the tectonic stress tensor from slip along faults and that obey the Coulomb yield condition. Tectonics, 6, 846-861.
Riedel, W., 1928. Zur Mechanik geologisher Brucherscheinungen. Zentralblatt für Geologie und Paleontologie Abhandlung, 13, 354-368.
Scholz, C.H., 2003. The mechanics of earthquakes and faulting. Cambridge University Press, 471.
Sintubin, M., van Noorden M. & Berwouts I., 2008. Late Devonian-Early Carboniferous contraction-dominated deformation in Central Armorica (Mont D’Arrée, Brittany, France) and its relationship with the closure of the rheic Ocean. Tectonophysics, 461, 343-355.
Srivastava, D.C., Lisle R. J. & Vandycke S., 1995. Shear zones as a new type of palaeostress indicator. Journal of Structural Geology, 17, 5, 663-676.
Strachan, R.A., Treloar P. J., Brown M. & D’Lemos R. S., 1989. Short Paper: Cadomian terrane tectonics and magmatism in the Armorican Massif. Journal of the Geological Society, London, 146, 423-426.
Tchalenko, J.S., 1970. Similarities between shear zones of different magnitudes. Geological Society of America Bulletin, 81, 1625-1640.
Van Noten, K., Muchez P. & Sintubin M., 2011. Stress-state evolution of the brittle upper crust during compressional tectonic inversion as defned by successive quartz vein-types (High-Ardenne slate belt, Germany). Journal of the Geological Society, London, 168, 2, 407-422.
Van Noten, K., Van Baelen H. & Sintubin M., 2012. The complexity of 3D stress-state changes during compressional tectonic inversion at the onset of orogeny. Geological Society, London, Special Publications, 367, 51-69.
Watts, M.J. & Williams G. D., 1979. Fault rocks as indicators of progressive shear deformation in the Guingamp region, Brittany. Journal of Structural Geology, 1, 4, 323-332.
Wilson, R.W., McCaffrey K. J. W., Holdsworth R. E., Imber J., Jones R. R., Welbon A. I. & Roberts D., 2006. Complex fault patterns, transtension and structural segmentation of the Lofoten ridge, Norwegian Margin: Using digital mapping to link onshore and offshore geology. Tectonics, 25, 1-28.