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Autor Andeweg, Bernd |
Documentos disponibles escritos por este autor (5)
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Vicente Muñoz, Gerardo de ; Martín Velázquez, Silvia ; Rodríguez Pascua, Miguel Angel ; Muñoz Martín, Alfonso ; Arcila, M. ; Andeweg, Bernd | Sociedad Geológica de España. | 2000The orientation of the principal stresses and the principal stress difference ratio has been determined along the southwestern boundary of the Euroasiatic plate with Northamerican and African plates by inversion method of focal mechanisms of ear[...]texto impreso
Vicente Muñoz, Gerardo de ; Martín Velázquez, Silvia ; Rodríguez Pascua, Miguel Angel ; Muñoz Martín, Alfonso ; Arcila, M. ; Andeweg, Bernd | Sociedad Geológica de España. | 2000The orientation of the principal stresses and the principal stress difference ratio has been determined along the southwestern boundary of the Euroasiatic plate with Northamerican and African plates by inversion method of focal mechanisms of ear[...]texto impreso
Muñoz Martín, Alfonso ; Cloetingh, Sierd ; Vicente Muñoz, Gerardo de ; Andeweg, Bernd | 1998-05-10Three subsequent Tertiary paleostress fields that are deduced from fault-slip data for the eastern part of the Tajo Basin are analyzed by finite-element studies. The modelling results show that maximum horizontal stresses (SHmax) are mainly cont[...]texto impreso
Cloetingh, Sierd ; Burov, E. ; Beekman, Fred ; Andeweg, Bernd ; Andriessen, Paul ; García Castellanos, Daniel ; Vicente Muñoz, Gerardo de ; Vegas, Ramón | 2002-10Integration of stress indicator data, gravity data, crustal kinematics data, and analysis of topography and recent vertical motions demonstrates the occurrence of consistently oriented spatial patterns of large-scale Alpine to recent intraplate [...]texto impreso
Andeweg, Bernd ; Vicente Muñoz, Gerardo de ; Cloetingh, Sierd ; Giner, Jorge ; Muñoz Martín, Alfonso | 1999Tertiary to present deformation in the interior of the Iberian Peninsula reflects spatial and temporal variations of the activity of the plate boundaries. Local deformation patterns observed in many of the numerous intraplate Tertiary basins and[...]