Titlebook: Geodynamics of Azores-Tunisia; E. Buforn,J. Martín-Dávila,A. Udías Book 2004 Springer Basel AG 2004 Deformation.Geodesy.Seismology.Seismot

強(qiáng)壯

notion

Iatrogenic

,Recent Tectonic Deformations and Stresses in the Frontal Part of the Rif Cordillera and the Sa?ss Bcement of the Ridges produced extensional deformation and the development of the Sa?ss foreland basin. The extension in this basin is oblate and features a well determined NNE-SSW trend near the Ridges, whereas it becomes prolate and pluridirectional near the foreland edge represented by the Rabat r

opportune

Recent Tectonic Structures in a Transect of the Central Betic Cordillera, reverse faults are mainly concentrated in the northern mountain front. However, normal faults affect the southern part of the Cordillera and are associated with the development of large asymmetrical basins such as the Granada Depression. In this setting, the slip along the crustal detachment is var

Obsequious

GEOALGAR Project: First Results on Seismicity and Fault-plane Solutions,that in the old solution; for the more regional events, the hypocenters corrections are bigger, with the focus becoming more shallow..Fault-plane solutions for the recent events were also estimated, showing that best solutions are dominated by strike-slip movement consistent with a stress controlled

外形

The Ain Temouchent (Algeria) Earthquake of December 22nd, 1999,Scalar seismic moment and source dimension have been obtained from spectral analysis. Results show thrust motion, with a horizontal pressure axis oriented in a NW-SE direction, a depth of 4 km and a simple source time function with time duration of 5 s. Scalar seismic moment estimated from waveform

消滅

Seismic Sources on the Iberia-African Plate Boundary and their Tectonic Implications,with E-W extension. Focal mechanisms of 26 intermediate-depth earthquakes in the Alboran Sea display vertical motions, with a predominant plane trending E-W. Solutions for very deep shocks correspond to vertical dip-slip along N-S trends. Frohlich diagrams and seismic moment tensors show different b

劇本

橡子

Geodetic Measurements of Crustal Deformation in the Western Mediterranean and Europe,y on the order of 1 mm/yr or better. Its analysis shows that Central Europe behaves rigidly at a 0.4 mm/yr level and can therefore be used to define a stable Europe reference frame. In that reference frame, we find that most of Europe, including areas west of the Rhine graben, the Iberian peninsula,

Prostaglandins