The ESCI-N Project after a decadeA synthesis of the results and open questions

Referencias bibliográficas

• Aller, J. (1993): Informe de la Campaña Gravimétrica, perfil escicantábrica-1. Informe interno, Dpto Geología, Univ. Oviedo, 14 pp.
• Alonso, J. L, Pulgar, J. A., García-Ramos, J. C. and Barba, P. (1996): Tertiary basins and Alpine tectonics in the Cantabrian Mountains (NW Spain). In: Tertiary basins of Spain: the stratigraphic record of crustal kinematics (P. F. Friend and C. J. Dabrio, Eds.), Cambridge University Press, Cambridge: 214-227.
• Álvarez-Marrón, J., Pérez-Estaún, A., Dañobeitia, J. J., Pulgar, J. A., Martínez-Catalán, J. R., Marcos, A., Bastida, F., AyarzaArribas, P., Aller, J., Gallart, J., González-Lodeiro, F., Banda. E., Comas, M. C. and Córdoba, D. (1996): Seismic structure of the northern continental margin of Spain from ESCIN deep seismic profiles. Tectonophysics, 264: 153-174.
• Álvarez-Marrón, J., Rubio, E. and Torné, M. (1997): Subductionrelated structures in the North Iberian Margin.J. Geophys. Res., 102: 2497-2511.
• Álvarez-Marrón, J., Pulgar, J. A., Dañobeitia, J. J., Pérez-Estaún, A., Gallastegui, J., Martínez-Catalán, J. R., Banda, E., Comas, M. C. and Córdoba, D. (1997a): Results from the ESCIN4 marine deep seismic profile in the northern Iberian margin. Rev. Soc. Geol. España, 8 (4), 1995: 355-363.
• Álvarez-Marrón, J., Pérez-Estaún, A., Dañobeitia, J. J., Pulgar, J. A., Martínez-Catalán, J. R., Marcos, A., Bastida, F., Aller, J., Ayarza-Arribas, P., Gallart, J., González-Lodeiro, F., Banda. E., Comas, M. C. and Córdoba, D. (1997b): Results from the ESCIN3.1 and ESCI-N3.2 marine deep seismic profiles in the northwestern Galicia margin. Rev. Soc. Geol. España, 8 (4), 1995: 331-339.
• Ayarza, P. (1995): Procesado, interpretación y modelado del perfil de reflexión profunda ESCIN-3.3. (Zonas Asturoccidental-Leonesa y Centro Ibérica). Tesis doctoral, 354 pp. Univ. de Salamanca.
• Ayarza, P., Martínez-Catalán, J. R., Gallart, J., Pulgar, J. A. and Dañobeitia, J. J. (1998): Estudio sísmico de la corteza ibérica norte 3.3: a seismic image of the Variscan crust in the hinterland of the NW Iberian Massif. Tectonics, 17: 171-186.
• Ayarza, P., Martínez-Catalán, J. R., Álvarez-Marrón, J., Zeyen, H. and Juhlin, C. (2004): Geophysical constraints on the deep structure of a limited ocean-continent subduction zone at the North Iberian Margin. Tectonics, 23, TC1010, doi: 10.1029/2002TC001487.
• Boillot, G., Dupeuble, P. A. and Malod, J. (1979): Subduction and tectonics on the continental margin off northern Spain. Mar. Geol.,32: 53-70.
• Cabal, J. (1993): Régimen térmico en el Noroeste de la Península Ibérica y sus márgenes continentales: flujo de calor, producción radiogénica de calor y estructura térmica de la litosfera.Tesis doctoral, 187 pp. Universidad de Oviedo.
• Choukroune, P. and ECORS Team (1989): The ECORS Pyrenean deep seismic profiles reflection data and the overall structure of an orogenic belt. Tectonics, 8(1): 23-39.
• Cloos, M. (1993): Lithospheric buoyancy and collisional orogenesis: subduction of oceanic plateaus, continental margins, island arcs, spreading ridges and seamounts. Geol. Soc. Am. Bull., 105: 715-737.
• Córdoba, D., Banda, E. and Ansorge, J. (1987): The Hercynian crust in northwestern Spain: a seismic survey. Tectonophysics,132: 321-333.
• Daignieres, M., De Cabissole, B., Gallart, J., Hirn, A., Suriñach, E. and Torné, M. (1989): Geophysical constraints on the deep structure along the Ecors Pyrenees line. Tectonics, 8: 1051-1058.
• Deregnaucourt, D. et Boillot, G. (1982): Structure geologique du Golfe de Gascogne. Bull. Bur. Geol. Min. France, 2(I): 149-178.
• England, P., Engdahl, R. and Thatcher, W. (2004): Systematic variation in the depths of slabs beneath arc volcanoes. Geophys. J. Int., 156: 377-408.
• Etude Continentale et Océanique par Réflexion et Réfraction Sismique (ECORS) Pyrénées Team (1988): The ECORS deep seismic reflection survey across the Pyrenees. Nature, 331: 508-511.
• Fernández Viejo, G. (1997): Estructura cortical de la Cordillera Cantábrica y su transición a la Cuenca del Duero a partir de datos de sísmica de refracción/reflexión de gran ángulo.Tesis doctoral, 316 pp., Univ. de Barcelona-CSIC.
• Fernández Viejo, G., Gallart, J., Pulgar, J. A., Córdoba, D. and Dañobeitia, J. J. (2000): Seismic signature of Variscan and Alpine tectonics in NW Iberia: Crustal structure of the Cantabrian Mountains and Duero basin. J. Geophys. Res.,105(B2) 3001-3018.
• Fernández Viejo, G., Gallart, J., Pulgar, J. A., Gallastegui, J., Dañobeitia, J. J. and Córdoba, D. (1998): Crustal transition between continental and oceanic domains along the North Iberian margin from wide angle seismic and gravity data. Geophys. Res. Let., 25(23): 4249- 4252.
• Fischer, K. M. (2004): Waning buoyancy in the crustal roots of old mountains. Nature, 417: 933-936. Flor, G. (1983): Las rasas asturianas: ensayos de correlación y emplazamiento. Trabajos de Geología, 13: 65-81.
• Gallart, J., Fernández Viejo, G., Díaz, J., Vidal, N., and Pulgar, J. A. (1997): Deep structure of the transition between the Cantabrian Mountains and the North Iberian margin from wide-angle ESCI-N data. Rev. Soc. Geol. España, 8 (4), 1995: 365-382.
• Gallastegui, J. (2000): Estructura cortical de la Cordillera y Margen continental Cantábricos: Perfiles ESCI-N. Trabajos de Geología22: 1-221.
• Gallastegui, J., Pulgar, J. A. andÁlvarez-Marrón, J. (1997): 2- D seismic modelling of the Variscan foreland thrust and Fold belt crust in NW Spain from ESCIN-1 deep seismic reflection data. Tectonophysics, 269: 21-32.
• Gallastegui, J., Pulgar, J. A. andGallart, J. (2002): Initiation of and active margin at the North Iberian continent-ocean transition. Tectonics, 21(4), 10.1029/2001TC901046.
• -Grimaud, S., Boillot, B., Collette, B. J., Mauffret, A., Miles P. R. and Roberts, D. B. (1982): Western extension of the Iberian-European plate boundary during the Early Cenozoic /Pyrenean) convergence: a new model. Mar. Geol., 45: 63-77.
• Hirn, A., Lepine, J., Jobert, G., Sapin, M., Wittlinger, G., XIN, X. Z., Yuan, G. E., Jing, W. X., Wen, T. J., Bai, X. S., Pandey, M. R. and Tater, J. M. (1984): Crustal structure and variability of the Himalayan border of the Tibet. Nature, 307: 23-25.
• Le Pichon, X., Bonnin, J. C., Francheteau, J. and Sibuet, J. C. (1971): Une hypothèse d’évolution tectonique du Golfe de Gascogne. In: Histoire structurale du Golfe de Gascogne.(J. Debysier, X. Le Pichon and M. Montadert, Eds.). Technip, París: VI11.1-VI11.44.
• Malod, J. A., Boillot, G., Capdevila, R., Dupeuble, P. A., Lepvrier, C., Mascle, G., Muller, C. and Taugordeau-Lanz, J. (1982): Subduction and tectonics on the continental margin off northern Spain: observations with the submersible Cyanna. In: Trench fore-arc geology (J. K. Legget, Ed.): Geological society of London, Special Publications, 10: 309-315.
• Martínez-Catalán, J. R., Ayarza-Arribas, P., Pulgar J. A., Pérez-Estaún, A., Gallart, J., Marcos, A., Bastida, F., Álvarez-Marrón, J., González-Lodeiro, F., Aller, J., Dañobeitia, J. J., Banda. E., Córdoba, D. and Comas, M. C. (1997): Results from the ESCI-N3.3 marine deep seismic profile along the Cantabrian continental margin.Rev. Soc. Geol. España, 8 (4), 1995: 341-354.
• Matte, P. (1991): Accretionary history and crustal evolution of the Variscan belt in Western Europe. Tectonophysics, 196: 279-287.
• Matte, P. andHirn, A. (1988): Seismic signature and tectonic crosssection of the Variscan crust in Western France. Tectonics, 7(2): 144-?
• Meissner, R., Wever, T. and Flueh, E. R. (1987): The Moho in Europe. Implications for crustal development. Ann. Geophys., B5: 357-364.
• Meissner, R., Weber, Th. and Sadowiak, P. (1990): Continental collisions and seismic signature. Geophys. J. Int., 102: 15-23.
• Montadert, L., Roberts, D. G., De Charpal, O., Guennoc, P. et al., (1979): Rifting and subsidence of the northern continental margin of the Bay of Biscay. In: Montadert, L. & Roberts, D. G. (Eds.).Initial Reports of the DSDP, 48. US Government Printing Office, Washington, D.C., 1025-1060.
• Moore, V. M. and Wiltschko, D. V. (2004): Syncollisional delamination and tectonic wedge development in convergent orogens. Tectonics, 23, TC2005, doi: 10.1029/2002TC001430.
• Morgan, P. and Burke, K. (1985): Collisional plateaus. Tectonophysics, 119: 137-151.
• Mueller, S. (1990): Intracrustal detachment and wedging along a detailed cross-section in central Europe. In: Exposed cross-sections of Continental crust (M. H. Salisbury and D. M. Fountain, Eds.). Kluwer Academic publishers: 623-643.
• Mueller, S. and Phillips, R. J. (1991): On the initiation of subduction. J. Geophys. Res., 96(B1): 651-665.
• Pedreira, D. (2004): Estructura cortical de la zona de transición entre los Pirineos y la Cordillera Cantábrica. Tesis doctoral, 343 pp., Univ. de Oviedo, 2004.
• Pedreira, D., Pulgar, J. A., Gallart, J., and Díaz, J. (2003): Seismic evidence of alpine crustal thickening and wedging from the western Pyrenees to the Cantabrian Mountains (north Iberia). J. Geophys. Res.,108(B4), doi: 10.1029/2001JB001667, 2003.
• Pérez-Estaún, A., Martínez-Catalán, J. R. and Bastida, F. (1991): Crustal thickening and deformation sequence in the footwall to the suture of the Variscan belt of Northwest Spain. Tectonophysics, 191: 243-253.
• Pérez-Estaún, A., Pulgar, J. A., Banda, E., Álvarez-Marrón, J. andESCIN Research Group (1994): Crustal structure of the external variscides in northwest Spain from deep seismic reflection profiling. Tectonophysics, 232: 91-118.
• Pous, J., Queralt, P. and Marcuello, A. (2001): Magnetotelluric signature of the western Cantabrian Mountains. Geophys. Res. Let., 28(9): 1795-1798.
• Prodehl, C. and Aichroth, B. (1992): Seismic investigations along the European Geotraverse and its surroundings in Central Europe. Terra Nova, 4(1): 14-24.
• Pulgar, J. A., Gallart, J., Fernández Viejo, G., Pérez-Estaún, A., Álvarez-Marrón, J. andESCIN Group (1996): Seismic image of the Cantabrian Mountains in the western extension of the Pyrenees from integrated ESCIN reflection and refraction data. Tectonophysics, 264: 1-19.
• Pulgar, J. A., Pérez-Estaún, A., Gallart, J., Álvarez-Marrón, J., Gallastegui, J., Alonso, J. L. and ESCIN Group (1997): The ESCI-N2 deep seismic reflection profile: a traverse across the Cantabrian Mountains and adjacent Duero basin.Rev. Soc. Geol. España, 8 (4), 1995: 383-394.
• Pulgar, J. A., Alonso, J. L, Espina, R. G. andMarín, J. A. (1999): La deformación alpina en el basamento varisco de la Zona Cantábrica. Trabajos de Geología, 21: 283-294.
• Sandwell, D. T. and Smith, W. H. F. (1997): Marine gravity anomalies from GEOSAT and ERS-I altimetry. J. Geophys. Res., 102: 10039-10054.
• Sacks, I. S. (1983): The subduction of young lithosphere. J. Geophys. Res., 88(B4): 3355-3366.
• Sibuet, J. C. and Le Pichon, X. (1971): Structure gravimetrique du Golfe de Gascogne et le fosse marginal nord-espagnol. In: Historie structurale du Golfe de Gascogne (J. Debysier, X. Le Pichon and L. Montadert, Eds.). Technip, París: VI.9.1-VI9.18.
• Soler, R., López-Vilches, J. and Riaza, C. (1981): Petroleum geology of the Bay of Biscay. In: Petroleum geology of the continental shelf of North-West Europe (L. V. Illing and G. D. Hobson, Eds.) The Inst. of Petrol., London: 474-482.
• Srivastava, S. P., Roest, W. R., Kovacs, L. C., Oakey, G., Levasque, S., Verhoef, J. and Macnab, R. (1990): Motion of Iberia since the Late Jurassic: Results from detailed aeromagnetic measurements in the Newfoundland basin. Tectonophysics,184: 229- 260.
• Stern, R. J. (2004): Subduction initiation: spontaneous and induced. Earth and Planet. Sci. Let., 226: 275-292.
• Téllez, J., Matías, L. M., Córdoba, D. and Mendes-Víctor, L. A. (1993): Structure of the crust in the schistose domain of Galicia-TrasOs-Montes (NW Iberian Peninsula). Tectonophysics, 221: 81-93.
• Williams, C. A. (1975): Sea-floor spreading in the Bay of Biscay and its relationship to the North Atlantic. Earth and Planet. Sci. Let., 24: 440-456.