Sustained post‐seismic effects on groundwater flow in fractured carbonate aquifers in Central Italy
A sustained increase in spring discharges was monitored after the 2016 Central Italy seismic
sequence in the fractured carbonate aquifer of Valnerina–Sibillini Mts. The groundwater …
sequence in the fractured carbonate aquifer of Valnerina–Sibillini Mts. The groundwater …
Localized afterslip at geometrical complexities revealed by InSAR after the 2016 Central Italy seismic sequence
L Pousse‐Beltran, A Socquet… - Journal of …, 2020 - Wiley Online Library
Abstract The Mw 6.5 Norcia earthquake occurred on 30 October 2016, along the Mt Vettore
fault (Central Apennines, Italy), it was the largest earthquake of the 2016–2017 seismic …
fault (Central Apennines, Italy), it was the largest earthquake of the 2016–2017 seismic …
Transient poroelastic response to megathrust earthquakes: a look at the 2015 Mw 8.3 Illapel, Chile, event
Large earthquakes can alter regional groundwater pressure, resulting in fluid flow, and the
process of restoring hydrostatic equilibrium would in turn lead to observable surface …
process of restoring hydrostatic equilibrium would in turn lead to observable surface …
Fluid-triggered aftershocks in an anisotropic hydraulic conductivity geological complex: The case of the 2016 Amatrice sequence, Italy
V Convertito, R De Matteis, L Improta… - Frontiers in Earth …, 2020 - frontiersin.org
The mechanism by which faults interact each other is still a debated matter. One of the main
issues is the role of pore-pressure diffusion in the delayed triggering of successive events …
issues is the role of pore-pressure diffusion in the delayed triggering of successive events …
Intrinsic and scattering seismic wave attenuation in the Central Apennines (Italy)
Recently, an earthquake sequence formed by a series of subsequences characterized by
large earthquakes (three events M≥ 6.0 and five events M≥ 5.0) occurred in the Central …
large earthquakes (three events M≥ 6.0 and five events M≥ 5.0) occurred in the Central …
Numerical analysis of interseismic, coseismic and post-seismic phases for normal and reverse faulting earthquakes in Italy
The preparation, initiation and occurrence dynamics of earthquakes in Italy are governed by
several frequently unknown physical mechanisms and parameters. Understanding these …
several frequently unknown physical mechanisms and parameters. Understanding these …
Influence of fault system geometry and slip rates on the relative role of coseismic and interseismic stresses on earthquake triggering and recurrence variability
C Sgambato, JP Faure Walker… - Journal of …, 2023 - Wiley Online Library
We model Coulomb stress transfer (CST) due to 30 strong earthquakes occurring on normal
faults since 1509 CE in Calabria, Italy, including the influence of interseismic loading, and …
faults since 1509 CE in Calabria, Italy, including the influence of interseismic loading, and …
Three-dimensional finite-element modeling of Coulomb stress changes on normal and thrust faults caused by pore fluid pressure changes and postseismic …
J Peikert, A Hampel, M Bagge - Geosphere, 2024 - pubs.geoscienceworld.org
The analysis of Coulomb stress changes has become an important tool for seismic hazard
evaluation because such stress changes may trigger or delay subsequent earthquakes …
evaluation because such stress changes may trigger or delay subsequent earthquakes …
The attenuation mechanism of high-frequency seismic waves in the Palghar swarm earthquake source area in Western India
N Subhadra, M Shekar - Journal of Asian Earth Sciences, 2024 - Elsevier
We study attenuation of seismic waves in the source area of Palghar swarm in western part
of India. The intrinsic and scattering loss are separated using the Wennerberg method in the …
of India. The intrinsic and scattering loss are separated using the Wennerberg method in the …
Relative importance of poroelastic effects and viscoelastic relaxation for postseismic velocity fields after normal and thrust earthquakes: Insights from 2D finite-element …
J Peikert, A Hampel, M Bagge - Tectonophysics, 2022 - Elsevier
Earthquakes on faults in the brittle upper crust evoke sudden changes in pore fluid pressure
as well as postseismic viscoelastic flow in the lower crust and lithospheric mantle but the …
as well as postseismic viscoelastic flow in the lower crust and lithospheric mantle but the …