We use continuous and survey GNSS data to image the spatial and temporal evolution of
afterslip during the 2 months following the Mw 8.3 2015 Illapel earthquake. Our approach …

After large earthquakes, parts of the fault continue to slip for days to months during the
afterslip phase, a behaviour documented for many earthquakes. Yet, little is known about the …

Large subduction earthquakes induce complex postseismic deformation, primarily driven by
afterslip and viscoelastic relaxation, in addition to interplate relocking processes. However …

Based on subdaily kinematic GNSS solutions, the fault slip properties during the very early
postseismic phase after the 2021 M 8.2 Chignik earthquake are investigated in this paper …

We present coseismic slip and afterslip inversion models based on the same fault geometry
for the Mw 8.6 2005 Nias‐Simeulue earthquake at the Sumatran subduction zone. We …

In the literature, the inverted coseismic slip models from seismological and geodetic data for
the 2011 Tohoku-Oki earthquake portray significant discrepancies, in particular regarding …

It is well-established that the post-seismic slip results from the combined contribution of
seismic and aseismic processes. However, the partitioning between these two modes of …

We focus on the relation between seismic and total postseismic afterslip following the Maule
M w 8.8 earthquake on 2010 February 27 in central Chile. First, we calculate the cumulative …

Geodetic observations of surface displacements during and following earthquakes such as
the March 11, 2011 great Tohoku earthquake can be used to constrain the spatial extent of …

In this study, we present inter-, co-and post-seismic displacements observed in the 2015
Illapel earthquake area by Global Positioning System (GPS) and Synthetic Aperture Radar …