The 2006 slow slip event and nonvolcanic tremor in the Mexican subduction zone

From our measured dust polarization angles, we infer a magnetic field orientation projected onto the plane of the sky (POS) that is remarkably ordered over the full extent of the

It is necessary to better constrain the slip history of this area since modelizations show that the recurrence intervals become shorter when closer to a large interplate

Kostoglodov (2011), Seismic evidence of nonlinear crustal deformation during a large slow slip event in Mexico, Geophys.. Lett., 38,

We observe a correlation between velocity changes (for period band greater than 14 s) and tremor activity whereas no correlation exists between velocity changes and seismic noise

Comme il a été précisé plus haut, nous nous intéresserons à travers ce travail, non seulement au degré d’exposition, d’utilisation du français lors des

Repeated cross-correlations of ambient seismic noise indicate a long-term seismic velocity change associated with the 2006 M7.5 slow-slip event (SSE) in the Guerrero region,

[ 25 ] The peaks of NVT activity are not randomly dis- tributed with respect to the timing of the small anomalous displacements. Six of the peaks roughly border the anoma- Table 2..

The four molecules chosen to demon- strate the inversion tunneling effects are ammonia with its umbrella motion during which the nitrogen atom passes from one side of the plane