MM
Member Since 2010
Marco Maria Scuderi
Post-Doc, Sapienza University of Rome
AGU Research
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The Effect of Normal Stress Oscillations on Fault Slip Behavior Near the Stability Transition From Stable to Unstable Motion
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
13 february 2024
Federico Pignalberi, Carolina Giorgetti, Corentin ...
Tectonic fault zones are subject to normal stress variations with a wide range of spatio‐temporal scales. Stress perturbations cover a wide r...
Seismicity Distribution within a Rheologically Heterogeneous Deformation zone: Insights from the Central Apennines.
EARTHQUAKE SOURCE CHARACTERIZATION AND FAULT ZONE PROPERTIES FROM MICROMETER TO KILOMETER SCALES III POSTER
seismology | 12 december 2023
Giuseppe Volpe, Giacomo Pozzi, Maria Eugenia Locch...
Although rheological heterogeneities are invoked to explain differences in fault slip behavior, case studies where an interdisciplinary approach is fo...
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The Effect of Shear Displacement and Wear on Fault Stability: Laboratory Constraints
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
01 april 2023
Corentin Noel, Carolina Giorgetti, Marco Maria Scu...
Faults are composed of a damage zone and a fault core with wear material that has accumulated during sliding. Fault zone width and structural compl...
Acoustic signature of fault slip from slow to fast earthquake: a laboratory insight
FROM ROCK PHYSICS TO EARTHQUAKE MECHANICS: INSIGHTS FROM THE FIELD, THE LAB, AND IN BETWEEN II POSTER
mineral and rock physics | 15 december 2022
Federico Pignalberi, Marco Maria Scuderi, Carolina...
In the last decades, it has been observed that faults can slip both by slow aseismic creep and seismic events (i.e., earthquakes). In between these tw...
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The effect of normal stress oscillations on the slip behavior of a critically stable fault
COMPARATIVE INVESTIGATIONS OF SLOW-TO-FAST EARTHQUAKES: OBSERVATIONS, EXPERIMENTS, AND NUMERICAL MODELING V ORAL
tectonophysics | 15 december 2022
Federico Pignalberi, Marco Maria Scuderi, Corentin...
Tectonic fault zones are subject to normal stress variations with a wide range of spatiotemporal scales, resulting in stress field alteration. These p...
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Hydromechanical Coupling at the Origin of Fault Slip Stability
PHYSICAL PROPERTIES OF EARTH MATERIALS (PPEM): FROM MICRO TO MACRO AND BACK AGAIN I ORAL
mineral and rock physics | 12 december 2022
Carolina Giorgetti, Marco Maria Scuderi, Christoph...
Hydromechanical heterogeneities of fault rocks control the potential for stable vs. unstable fault slip behavior. These heterogeneities arise from the...
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The Role of Fault Rock Fabric in the Dynamics of Laboratory Faults
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
07 june 2022
Giacomo Pozzi, Marco Maria Scuderi, Elisa Tinti, M...
Fault stability is inherently linked to the frictional and healing properties of fault rocks and associated fabrics. Their complex interaction cont...
Bifurcations at the Stability Transition of Earthquake Faulting
FAULT-SLIP ACCELERATION: FROM SLOW TO FAST, FROM THE LAB TO THE FIELD, AND IN BETWEEN I ORAL
mineral and rock physics | 15 december 2021
Deepa Mele Veedu, Carolina Giorgetti, Marco Maria ...
Tectonic faults typically break in a single rupture mode within the range of styles from slow slip to dynamic earthquake failure. However, in increasi...
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