ABSTRACT
Built-up on top of ancient lake deposits, Mexico City experiences some of the largest seismic site effects worldwide. Besides the extreme amplification of seismic waves, duration of intense ground motion from large subduction earthquakes exceeds three minutes in the lake-bed zone of the basin, where hundreds of buildings collapsed or were seriously damaged during the magnitude 8.0 Michoacán earthquake in 1985. Different mechanisms contribute to the long lasting motions, such as the regional dispersion and multiple-scattering of the incoming wavefield from the coast, more than 300 km away the city. By means of high performance computational modeling we show that, despite the highly dissipative basin deposits, seismic energy can propagate long distances in the deep structure of the valley, promoting also a large elongation of motion. Our simulations reveal that the seismic response of the basin is dominated by surface-waves overtones, and that this mechanism increases the duration of ground motion by more than 170% and 290% of the incoming wavefield duration at 0.5 and 0.3 Hz, respectively, which are two frequencies with the largest observed amplification. This conclusion contradicts what has been previously stated from observational and modeling investigations, where the basin itself has been discarded as a preponderant factor promoting long and devastating shaking in Mexico City.
ABSTRACT
Mt. Vesuvius is a small volcano associated with an elevated risk. Seismic data were used to better define its magmatic system. We found evidence of an extended (at least 400 square kilometers) low-velocity layer at about 8-kilometer depth. The inferred S-wave (approximately 0.6 to 1.0 kilometer per second) and P-wave velocities (approximately 2.0 kilometer per second) as well as other evidence indicate an extended sill with magma interspersed in a solid matrix.
ABSTRACT
Since 1994, important modifications have been implemented in the dental curriculum in France, and an additional year has been included in the dental curriculum. The 1st year has remained unchanged; it is common to both medical and dental schools and leads to a selection procedure of 1 in 10 dental students. In the new curriculum, the dental student is engaged in a 5-year programme in dental school (years 2 to 6), as opposed to 4 years in the former programme (years 2 to 5). Basically, this new curriculum emphasises research initiation, links with medical training and offers broader clinical experience. During the academic year 1998-1999, dental schools had 2 different types of students: the 4th year students belonging to the new programme along with the 5th year students in their final year of the old curriculum. Using a specially devised questionnaire, we investigated the students' perception of their respective training, their motivation and professional plans. At the Faculty of Odontology in Lyon, the new curriculum is perceived as an increased strain by the dental students.
