• Aucun résultat trouvé

Spatial and temporal evolution of a long term slow slip event: the 2006 Guerrero Slow Slip Event

N/A
N/A
Protected

Academic year: 2021

Partager "Spatial and temporal evolution of a long term slow slip event: the 2006 Guerrero Slow Slip Event"

Copied!
14
0
0

Texte intégral

Loading

Figure

Figure 1. Seismotectonic map [after Kostoglodov et al. (2003)] and GPS station location (black triangles)
Figure 2. North, East and Vertical GPS time series for all analysed stations in this study (from Vergnolle et al
Figure 3. Geometry of the fault plane used in this study along a profile perpendicular to the trench (adapted from P´erez-Campos et al
Figure 4. (a) Slip distribution resulting from the inversion of GPS cumulative displacements
+6

Références

Documents relatifs

Consistent with a beneficial role of sleep for memory consolidation, participants who slept after learning exhibited a significantly improved cued recall performance after the 12-hr

The nonmodal stability analysis, however, reveals that slip has a very weak influence on the maximum transient energy growth of perturbations at subcritical Reynolds numbers..

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,

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

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

Mechanistic Studies on Pd-Catalyzed Fluorination of Cyclic Vinyl Triflates: Evidence for in situ Ligand Modification by TESCF 3 as an Additive 2 .1 Introduction

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