4 citations · 5 across the 6 of their papers we have counts for
6 papers
A systematic search for tectonic tremor and low-frequency earthquakes in the Atacama segment of the Chilean subduction zone (24S-31S) turns up empty
Jannes Münchmeyer, William B. Frank, Sophie Giffard-Roisin +2
Subduction megathrusts release stress not only seismically through earthquakes, but also through creep and transient slow deformation, called slow slip events (SSEs). Understanding…
Characterising the Atacama segment of the Chile subduction margin (24°S-31°S) with >165,000 earthquakes
Jannes Münchmeyer, Diego Molina-Ormazabal, David Marsan +8
The Atacama segment in Northern Chile (24°S to 31°S) is a mature seismic gap with no major event (Mw>8) since 1922. In addition to regular seismicity, around the subducting Copiapó…
Seismic swarms unveil the mechanisms driving shallow slow slip dynamics in the Copiapó ridge, Northern Chile
Jannes Münchmeyer, Diego Molina, Mathilde Radiguet +6
Like earthquakes, slow slip events release elastic energy stored on faults. Yet, the mechanisms behind slow slip instability and its relationship with seismicity are debated. Here,…
Denoising of Geodetic Time Series Using Spatiotemporal Graph Neural Networks: Application to Slow Slip Event Extraction
Giuseppe Costantino, Sophie Giffard-Roisin, Mauro Dalla Mura +1
Geospatial data has been transformative for the monitoring of the Earth, yet, as in the case of (geo)physical monitoring, the measurements can have variable spatial and temporal sa…
Deep learning detects uncataloged low-frequency earthquakes across regions
Jannes Münchmeyer, Sophie Giffard-Roisin, Marielle Malfante +4
Documenting the interplay between slow deformation and seismic ruptures is essential to understand the physics of earthquakes nucleation. However, slow deformation is often difficu…
Slow slip detection with deep learning in multi-station raw geodetic time series validated against tremors in Cascadia
Giuseppe Costantino, Sophie Giffard-Roisin, Mathilde Radiguet +3
Slow slip events (SSEs) originate from a slow slippage on faults that lasts from a few days to years. A systematic and complete mapping of SSEs is key to characterizing the slip sp…