Skip to main content
Log in

Stress fields in the Iberian-Maghrebi region

  • Published:
Journal of Seismology Aims and scope Submit manuscript

Abstract

This study concerns the present stressfield between the Eurasian and Africanplates in the Iberian-Maghrebi region(Portugal, Spain, Morocco, Algeria andTunisia). In addition to an up-to-datecatalogue of earthquakes in this area, acatalogue of the focal mechanisms composedof 486 solutions of fault planes,standardized in terms of notation andinformation type, was used. These data wereused applying the right-dihedron method ofAngelier and Mechler (1977), to obtaindifferent zones with homogeneous stress.The results obtained for shallowearthquakes (h < 30 km) coincide, in themajority of cases, with the general stressfields proposed by numerous authors forthis region, according to which there isNW-SE compression. However, the stressorientation appears to vary in certainareas, perhaps perturbed by the opening ofthe Atlantic Ocean, the approach of Iberiaand Africa, or the extension of the AlboranSea.For the intermediate earthquakes (30 < h< 150 km) no general pattern was found,and the P and T axes seem to be randomlyoriented for the depth intervalsconsidered. For the very deep earthquakes(h > 600 km), however, the P axis lies ina NNW-SSE direction, dipping towards theSSE, while the T axis is subhorizontal in aNE-SW direction.The determinations from the focalmechanisms highlight the existence of aregional stress field with a subhorizontalcompression axis trending NW-SE. Superimposed are others that specificallyaffect particular sectors; these arerelated to the opening of the AtlanticOcean, the extension of the BeticCordillera and the Alboran Sea, and eventhe present compression between the Iberianand European plates.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Alfaro, P., Rueda, J., Delgado, J., Estévez, A., López Casado, C. and Giner, J., 1999, Sismotectónica de la cuenca del bajo Segura (Cordillera Bética central, Proc. 1a Asamblea Hispano Portuguesa de Geodesia y Geofísica. Almeria. Ed. Universidad de Almería and Instituto Geográfico Nacional. España.

    Google Scholar 

  • Andrieux, J., Fontboté, J.M. and Mattauer, M., 1971, Sur un modèle explicatif de l'Arc de Gibraltar, Earth Plan. Sci. Lett. 12, pp. 191–198.

    Google Scholar 

  • Andrieux, J. and Mattauer, M., 1973, Précisions sur un modèle explicatif de l'Arc de Gibraltar, Bull. Soc. géol. France (7)XV, pp. 115–118.

    Google Scholar 

  • Angelier, J. y Mechler, P., 1977, Sur une méthode graphique de recherche des contraintes principales egalement utilisable en tectonique et en seismologie: la methode des diedres droites, Bull. Soc. géol. France 7(19), 1309–1318.

    Google Scholar 

  • Araña, V. and Vegas, R., 1974, Plate tectonics and volcanism in the strait of Gibraltar, Tectonophysics 24, 197–212.

    Google Scholar 

  • Bezzeghoud, M. and Buforn, E., 1999, Source Parameters of the 1992 Melilla (Spain, M W = 4.8), 1994 Alhoceima (Morocco, M W = 5.8), and 1994 Mascara (Algeria, M W = 5.7) Earthquakes and Seismotectonic Implications, Bull. Seism. Soc. Am. 89(2), 359–372.

    Google Scholar 

  • Blanco, M.J. and Spackman, W., 1993, The P-wave velocity structure of the mantle below the Iberian Peninsula: Evidence for subduction lithophere below southern Spain, Tectonophysics 221, 13–34.

    Google Scholar 

  • Brillinger, D.R., Udías, A. and Bolt, B.A., 1980, A probability model for regional focal mechanism solutions, Bull. Seism. Soc. Am. 70(1), 149–170.

    Google Scholar 

  • Buforn, E., Udías, A. and Mezcua, J., 1988a, Seismicity and focal mechanisms in south Spain, Bull. Seism. Soc. Am. 78(6), 2008–2024.

    Google Scholar 

  • Buforn, E., Udías, A. and Colombás, M.A., 1988b, Seismicity, source mechanisms and tectonics of the Azores-Gibraltar plate boundary, Tectonophysics 152, 89–118.

    Google Scholar 

  • Buforn, E., Udías, A. and Madariaga, R., 1991, Intermediate and Deep Earthquakes in Spain, Pageoph 136, nÚm.4, 375–393.

    Google Scholar 

  • Buforn, E., Sanz de Galdeano, C. and Udías, A., 1995, Seismotectonics of the Ibero-Maghrebian region, Tectonophysics 248, 247–261.

    Google Scholar 

  • Buforn, E., Coca, P., Udías, A. and Lasa, C., 1997, Source mechanism of intermediate and deep earthquakes in southern Spain, J. Seismol. 1, 113–130.

    Google Scholar 

  • Calvert, A., Sandvol, E., Seber, D., Barazangi, M., Vidal, F., Alguacil, G. and Jabour, N., 2000, Propagation of regional seismica phases (Lg and Sn) and Pn velocity structure along the Africa-Iberia plate boundary zone: tectonic implications, Geophys. J. Int. 142, 384–408.

    Google Scholar 

  • Coca, P. and Buforn, E., 1994, Mecanismos focales en el sur de España: Periodo 1965–1985, Estudios Geológicos 50, 33–45.

    Google Scholar 

  • Cortés, A.L. and Maestro, A., 1998, Recent intraplate stress field in the eastern Duero Basin (N Spain), Ter ra Nova 10, 287–294.

    Google Scholar 

  • Creager, C., Chiao, L.Y., Winchester, J.P., Engdahl, E.R., 1995, Membrane strain rates in the subducting plate beneath South America, Geophys. Res. Lett. 22, 2321–2324.

    Google Scholar 

  • DeMets, C., R. Gordon, D. Argus and S. Stein, 1990, Current plate motions, Geophys. J. Int. 101, 425–478.

    Google Scholar 

  • DeMets, C., R. Gordon, D. Argus and S. Stein, 1994, Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions, Geophys. Res. Lett. 21, 2191–2194.

    Google Scholar 

  • Galindo Zaldívar, J., González Lodeiro, F., and Jabaloy, A., 1993, Stress and palaeostress in the Betic-Rif cordilleras (Miocene to the present), Tectonophysics 227, 105–126.

    Google Scholar 

  • Galindo Zaldívar, J., Jabaloy, A., Serrano, I., Morales, J., González Lodeiro, F. and Torcal, F., 1999, Recent and present-day stresses in the Granada Basin (Betic Cordilleras): Example of a late Miocene-present-day extensional basin in a convergent plate boundary, Tectonics 18(4), 686–702.

    Google Scholar 

  • Giner Robles, J.L., 1996, Análisis Neotectónico y Sismotectónico en el Sector Centro-Oriental de la Cuenca del Tajo, Tesis Doctoral. Universidad Complutense de Madrid, 345 pp.

  • Grimison, N. and Chen, W., 1986, The Azores-Gibraltar Plate Boundary: Focal Mechanisms, Depths of Earthquakes and their Tectonic Implications, J. Geophys. Res. 91, 2029–2047.

    Google Scholar 

  • Henares Romero, J., López Casado, C. and Delgado J., 2000, Catalogue of focal mechanisms for the Iberian-Maghrebian region. 2a Asamblea Hispano Portuguesa de Geodesia y Geofísica. Lagos. Portugal.

  • Henares Romero, J. and López Casado, C., 2001, Catálogo de mecanismos focales del area Ibero-Mogrebí. In: C. López Casado (ed.), Reprodigital, Granada. ISBN 84-699-5695-7.

  • Herraiz, M., De Vicente, G., Lindo Ñaupari, R., Giner, J., Simón, J.L., González Casado, J.M., Vadillo, O., Rodríguez-Pascua, M.A., Cicuéndez, J.I., Casas, A., Cabañas, L., Rincón, P., Cortés, A.L., Ramírez, M. and Lucini, M., 2000, The recent (upper Miocene to Quaternary) and present tectonic stress distributions in the Iberian Peninsula, Tectonics 19, 762–786.

    Google Scholar 

  • Lisle, R.J., 1987, Principal stress orientations form faults: An additional constraint., Annales Tectonicae 1(2), 155–158.

    Google Scholar 

  • Lu, Z., Wiss, M., Pulpan, H., 1997, Details of stress directions in the Alaska subduction zone from fault plane solutions, J. Geophys. Res. 102, 5385–5402.

    Google Scholar 

  • Medina, F. and Cherkaoui, T.E., 1991, Focal mechanisms of the Atlas earthquakes, and tectonic implications., Geologische Rundschau 80/3, 639–648.

    Google Scholar 

  • Mezcua, J. and Rueda, J., 1997, Seismological evidence for a delamination process in the lithosphere under the Alboran Sea, Geophys. J. Int. 129, 256–264.

    Google Scholar 

  • Morales, J., Serrano, I., Vidal, F. and Torcal, F., 1997, The depth of the earthquake activity in the Central Betic (Southern Spain), Geophys. Res. Lett. 24, 3289–3292.

    Google Scholar 

  • Morales, J., Serrano, I., Jabaloy, A., Galindo-Zaldívar, J., Zhao, D., Torcal, F., Vidal, F. and González-Lodeiro, F., 1999, Active continental subduction beneath the Betic Cordillera and the Alborán Sea, Geology 27, 735–738.

    Google Scholar 

  • Moreira, V.S., 1985, Seismotectonics of Portugal and its adjacent area in the Atlantic, Tectonophysics 117, 85–96.

    Google Scholar 

  • Pegora, O., 1972, Application de la microtectonique à un étude de neotectonique. Le golfe Maliaque (Grèce centrale, Thèse troisième cycle. U.S.T.L. Montpellier. 41 pp.

  • Proyecto Sigma, 1998, Análisis del estado de esfuerzos tectónicos, reciente y actual a partir de poblaciones de fallas y mecanismos focales de terremotos. Metodología y aplicación a la Península Ibérica. Colección Otros Documentos, CSN, Madrid.

    Google Scholar 

  • Sanz de Galdeano, C., 1983, Los accidentes y fracturas principales de las Cordilleras Béticas, Estudios Geol. 39, 157–165.

    Google Scholar 

  • Sanz de Galdeano, C., 1990, Geologic evolution of the Betic Cordilleras in the Western Mediterranean, Miocene to the present, Tectonophysics 172, 107–119.

    Google Scholar 

  • Sanz de Galdeano, C., 1996, The E-W segments of the contact between the External and Internal Zones of the Betic and Rif Cordilleras and the E-W corridors of the Internal Zone (A combined explanation), Estudios Geológicos 52, 123–136.

    Google Scholar 

  • Sanz de Galdeano, C., 1997, La Zona Interna Bético-Rifeña (Antecedentes, unidades tectónicas, correlaciones y bosquejo de reconstrucción paleogeográfica). Monografía Tierras del Sur. Ed. Universidad de Granada, 316 pp.

  • Seber, D., Barazangi, M., Ibenbrahim, A. and Demnati, A., 1996a, Geophysical evidence for lithospheric delamination beneath the Alboran Sea and Rif-Betic mountains, Nature 379, 785–790.

    Google Scholar 

  • Seber, D., Barazangi, M., Tadili, B.A., Ramdani, M. and Ben Sari, D., 1996b, Three-dimensional upper mantle structure beneath the intraplate Atlas and interplate Rif mountains of Morocco, J. Geophys. Res. 101, 87, 3125–3138.

    Google Scholar 

  • Udías, A., 1982, Seismicity and seismotectonic stress field in the Alpine-Mediterranean region, Geodynamics Series 7, 75–82.

    Google Scholar 

  • Udías, A. and Buforn, E., 1991, Regional Stresses Along the Eurasia-Africa Plate Boundary Derived from Focal Mechanisms of Large Earthquakes, Pageoph 136(4), 433–448.

    Google Scholar 

  • Udías, A., López Arroyo, A. and Mezcua, J., 1976, Seismotectonic of the Azores-Alboran region Tectonophysics 31, 259–289.

    Google Scholar 

  • Van Bemmelem, R.W., 1969, Origin of the Western Mediterraneam Sea, Geol. Mijnbouw 26, 13–52.

    Google Scholar 

  • Van Bemmelem, R.W., 1972a, Driving forces of Mediterraneam Orogeny (Tyrrhenian Test-case, Geol. Mijnbouw 51(5), 548–573.

    Google Scholar 

  • Van Bemmelem, R.W., 1972b, Geodynamic models (an evaluation and a synthesis). Elsevier, Amsterdam, 267 pp.

    Google Scholar 

  • Van Bemmelem, R.W., 1973, Geodynamic models for the Alpine type of orogeny (Test-case II: The Alps in Central Europe), Tectonophysics 18, 33–79.

    Google Scholar 

  • Vissers, R.L.M., Platt, J.P. and Van der Wal, D., 1995, Late orogenic extension of the Betic Cordillera and the Alboran Domain: A lithospheric view, Tectonics 14(4), 786–803.

    Google Scholar 

  • Wang, K., Mulder, T., Rogers, G.C., Hydman, R.D., 1995, Case for very low coupling stress on the Cascadia subduction pfault, J. Geophys. Res. 100, 12907–12918.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Henares, J., López Casado, C., Sanz de Galdeano, C. et al. Stress fields in the Iberian-Maghrebi region. Journal of Seismology 7, 65–78 (2003). https://doi.org/10.1023/A:1021294015027

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1023/A:1021294015027

Navigation