An integrated perspective of the continuum between earthquakes and slow-slip phenomena
The discovery of slow-slip phenomena has revolutionized our understanding of how faults
accommodate relative plate motions. Faults were previously thought to relieve stress either …
accommodate relative plate motions. Faults were previously thought to relieve stress either …
From geodetic imaging of seismic and aseismic fault slip to dynamic modeling of the seismic cycle
JP Avouac - Annual Review of Earth and Planetary Sciences, 2015 - annualreviews.org
Understanding the partitioning of seismic and aseismic fault slip is central to seismotectonics
as it ultimately determines the seismic potential of faults. Thanks to advances in tectonic …
as it ultimately determines the seismic potential of faults. Thanks to advances in tectonic …
Deformation cycles of subduction earthquakes in a viscoelastic Earth
Subduction zones produce the largest earthquakes. Over the past two decades, space
geodesy has revolutionized our view of crustal deformation between consecutive …
geodesy has revolutionized our view of crustal deformation between consecutive …
Coseismic Slip and Afterslip of the Great Mw 9.15 Sumatra–Andaman Earthquake of 2004
We determine coseismic and the first-month postseismic deformation associated with the
Sumatra–Andaman earthquake of 26 December 2004 from near-field Global Positioning …
Sumatra–Andaman earthquake of 26 December 2004 from near-field Global Positioning …
Seismic and aseismic slip on the Central Peru megathrust
Slip on a subduction megathrust can be seismic or aseismic, with the two modes of slip
complementing each other in time and space to accommodate the long-term plate motions …
complementing each other in time and space to accommodate the long-term plate motions …
A viscoelastic and afterslip postseismic deformation model for the 1964 Alaska earthquake
H Suito, JT Freymueller - Journal of Geophysical Research …, 2009 - Wiley Online Library
We developed a 3‐D viscoelastic model, in concert with an afterslip model, to describe the
postseismic deformation following the 1964 Alaska earthquake. Our model incorporates a …
postseismic deformation following the 1964 Alaska earthquake. Our model incorporates a …
Interseismic coupling, segmentation and mechanical behavior of the central Chile subduction zone
Global Positioning System (GPS) measurements carried out in Chile over the last two
decades showed that an entire portion of the Nazca‐South America subduction zone (38° …
decades showed that an entire portion of the Nazca‐South America subduction zone (38° …
Modeling afterslip and aftershocks following the 1992 Landers earthquake
H Perfettini, JP Avouac - Journal of Geophysical Research …, 2007 - Wiley Online Library
One way to probe the rheology of the lithosphere and fault zones is to analyze the temporal
evolution of deformation following a large earthquake. In such a case, the lithosphere …
evolution of deformation following a large earthquake. In such a case, the lithosphere …
Seismicity structure of the northern Chile forearc from> 100,000 double‐difference relocated hypocenters
In this study, we present high‐resolution seismicity images of the northern Chile subduction
zone forearc. We used 8 years of continuous seismic waveform data from the Integrated …
zone forearc. We used 8 years of continuous seismic waveform data from the Integrated …
Revisiting the North Chile seismic gap segmentation using GPS-derived interseismic coupling
No major earthquake occurred in North Chile since the 1877 M w 8.6 subduction earthquake
that produced a huge tsunami. However, geodetic measurements conducted over the last …
that produced a huge tsunami. However, geodetic measurements conducted over the last …