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Member Since 2014
Anne Socquet
Pr, ISTerre Institute of Earth Sciences
AGU Research
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Characterising the fine-structure of the Northern Chile subduction zone (24⁰S - 31⁰S) with > 160,000 earthquakes
FROM THE SURFACE TO THE MANTLE: INTEGRATING GEOPHYSICAL, SEISMOLOGICAL, AND TECTONICS PERSPECTIVES ALONG THE SOUTH AMERICAN MARGIN I POSTER
tectonophysics | 13 december 2024
Jannes Münchmeyer, Diego Molina, David Marsan, Mic...
The Chilean margin is one of the world's seismically most active zones. A known seismic gap is the Atacama segment (24⁰S - 31⁰S) with no major event (...
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Interseismic Coupling at the South Peru Subduction Zone and Impact of the Postseismic Relaxation Following the 2001 Mw8.4 Arequipa Earthquake
FROM THE SURFACE TO THE MANTLE: INTEGRATING GEOPHYSICAL, SEISMOLOGICAL, AND TECTONICS PERSPECTIVES ALONG THE SOUTH AMERICAN MARGIN I POSTER
tectonophysics | 13 december 2024
Bertrand Lovery, Anne Socquet, Mohamed Chlieh, Mat...
There is intense seismic activity at the Central Andes subduction zone, and good knowledge of interplate coupling and seismic cycles is important to i...
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Structure and seismicity of the Southern Peru subduction zone
FROM THE SURFACE TO THE MANTLE: INTEGRATING GEOPHYSICAL, SEISMOLOGICAL, AND TECTONICS PERSPECTIVES ALONG THE SOUTH AMERICAN MARGIN II ORAL
tectonophysics | 13 december 2024
Caroline Chalumeau, Sebastien Chevrot, Hugo Sánche...
The southern Peru subduction zone is a complex region, marking the transition between the flat slab associated with the Nazca Ridge subduction in the ...
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Slip-tremor interaction at the very beginning of Episodic Tremor and Slip in Cascadia
SLOW-TO-FAST EARTHQUAKES FROM SHALLOW TO DEEP: MULTISCALE RHEOLOGY OF PLATE BOUNDARY FAULTS V POSTER
seismology | 12 december 2024
Yuji Itoh, Anne Socquet, Mathilde Radiguet
In Cascadia, the concomitance of slow slip events (SSE) and tremors during Episodic Tremor and Slip (ETS) episodes is well documented. Brittle tremor ...
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A comprehensive search for low-frequency earthquakes and tectonic tremor along the Northern Chile subduction zone (24⁰S - 31⁰S)
SLOW-TO-FAST EARTHQUAKES FROM SHALLOW TO DEEP: MULTISCALE RHEOLOGY OF PLATE BOUNDARY FAULTS V POSTER
seismology | 12 december 2024
Jannes Münchmeyer, William B. Frank, Sophie Giffar...
Over the last three decades, a wide range of slow earthquakes have been detected in subduction zones, ranging from long-term slow slip events down to ...
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Deep and shallow slow slip events imaged by GNSS and seismicity in Copiapo ridge, Chile : kinematics and segmentation driven by interactions between fluids and subducted seamounts
SLOW-TO-FAST EARTHQUAKES FROM SHALLOW TO DEEP: MULTISCALE RHEOLOGY OF PLATE BOUNDARY FAULTS II ORAL
seismology | 11 december 2024
Anne Socquet, Diego Molina, Jannes Münchmeyer, Mat...
Like earthquakes, slow slip events contribute to the release of elastic energy stored on faults. They are usually associated with limited seismic radi...
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Continuous Monitoring of Slow Slip in Cascadia: Implications for Scaling Laws and Source Time Function
SLOW-TO-FAST EARTHQUAKES FROM SHALLOW TO DEEP: MULTISCALE RHEOLOGY OF PLATE BOUNDARY FAULTS I POSTER
seismology | 11 december 2024
Giuseppe Costantino, Mathilde Radiguet, Anne Socqu...
Slow slip has revolutionized our understanding of relative plate motions, shedding light on more complex processes of stress release in tectonic areas...
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Using Sentinel-1 Timeseries for Large-scale Tectonic Applications in Central Andes
RECENT ADVANCES IN SAR AND INSAR PROCESSING, BIG DATA ANALYSIS, AND EARTH SCIENCE APPLICATIONS I ORAL
geodesy | 11 december 2024
Bertrand Lovery, Marie-Pierre Doin, Mohamed Chlieh...
In order to study the large-scale deformation in Central Andes (726°S), we use InSAR Sentinel-1 acquisitions, processed in the frame of the FLATSIM-An...
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