The Transient and Intermittent Nature of Slow Slip

Afterwards, the uniqueness of the solution (volume change and drift rate) is enforced by minimizing the correlation between deformation model parameters

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

However, modeling saltation intermittency from a LES approach is still chal- lenging because saltation occurs near the surface, within a layer not exceeding 1 m height, where

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

Final moment, slip and rupture length with time for slow-slip events, earthquakes and nucleation phase of

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

Along the North Ih Bogd segment, we estimated the horizontal slip rate of the Bogd Fault at Bitut, a site located 40 km east of the the Noyan Uul site (Fig.. There, a system of

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,