su indicazione di Martina Rocca, si condivide il messaggio relativo alla sessione TS3.3 "From aseismic creep to dynamic earthquake rupture: the spectrum of fault slip mode across scales" che si terrà nell'ambito del congresso EGU 2026 (Vienna, 3-8 maggio 2026).
Conveners: Martina Rocca, Simone Masoch, Giuseppe Volpe.
Un caro saluto
La segreteria GIGS
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Dear Colleagues,
We are delighted to invite you to participate and contribute to our scientific session titled "From aseismic creep to dynamic earthquake rupture: the spectrum of fault slip mode across scales", scheduled for the EGU 2026 meeting held in Wien from May 3-8, 2026.
January 15, 2026 @ 13:00 CET is the deadline to submit your abstracts!
Session Overview: TS3.3 From aseismic creep to dynamic earthquake rupture: the spectrum of fault slip mode across scales (Co-organized by EMRP1/GD11).
Faults release tectonic strain through a wide and complex spectrum of slip behaviors, including aseismic creep, episodic slow-slip events and earthquakes.
Field observations, seismological data, laboratory experiments, and numerical modelling have demonstrated that a range of factors, including structural and geometrical complexity, mechanical and rheological heterogeneities, fluid pressure and chemistry, and temperature, interact in complex ways and play a critical role in controlling fault slip behavior. However, how these interconnected factors influence the occurrence and evolution of different slip modes as well as the transitions between them, remains yet a fundamental and unresolved challenge.
Call for Contributions: This session welcomes contributions that investigate the wide range of fault slip behaviours using multidisciplinary and multiscale approaches, including field and microstructural analyses of exhumed faults, laboratory experiments, geochemical characterization of fluids, seismological and geodetic observations of active faults, and numerical modelling. We aim to foster discussion on the physico-chemical processes governing fault strength, slip mode, and fault geometrical evolution, and how these insights improve seismic hazard assessment and our understanding of the mechanics of faulting and earthquake.
Conveners: Martina Rocca (Università di Milano-Bicocca), Simone Masoch (University of Nevada, Reno), Giuseppe Volpe (Università di Roma-La Sapienza)
More info here: https://meetingorganizer.copernicus.org/EGU26/session/56663
Looking forward to seeing you in Wien!
Martina Rocca, Simone Masoch, Giuseppe Volpe
We are delighted to invite you to participate and contribute to our scientific session titled "From aseismic creep to dynamic earthquake rupture: the spectrum of fault slip mode across scales", scheduled for the EGU 2026 meeting held in Wien from May 3-8, 2026.
January 15, 2026 @ 13:00 CET is the deadline to submit your abstracts!
Session Overview: TS3.3 From aseismic creep to dynamic earthquake rupture: the spectrum of fault slip mode across scales (Co-organized by EMRP1/GD11).
Faults release tectonic strain through a wide and complex spectrum of slip behaviors, including aseismic creep, episodic slow-slip events and earthquakes.
Field observations, seismological data, laboratory experiments, and numerical modelling have demonstrated that a range of factors, including structural and geometrical complexity, mechanical and rheological heterogeneities, fluid pressure and chemistry, and temperature, interact in complex ways and play a critical role in controlling fault slip behavior. However, how these interconnected factors influence the occurrence and evolution of different slip modes as well as the transitions between them, remains yet a fundamental and unresolved challenge.
Call for Contributions: This session welcomes contributions that investigate the wide range of fault slip behaviours using multidisciplinary and multiscale approaches, including field and microstructural analyses of exhumed faults, laboratory experiments, geochemical characterization of fluids, seismological and geodetic observations of active faults, and numerical modelling. We aim to foster discussion on the physico-chemical processes governing fault strength, slip mode, and fault geometrical evolution, and how these insights improve seismic hazard assessment and our understanding of the mechanics of faulting and earthquake.
Conveners: Martina Rocca (Università di Milano-Bicocca), Simone Masoch (University of Nevada, Reno), Giuseppe Volpe (Università di Roma-La Sapienza)
More info here: https://meetingorganizer.copernicus.org/EGU26/session/56663
Looking forward to seeing you in Wien!
Martina Rocca, Simone Masoch, Giuseppe Volpe